cometadata/datacite-rtg-text-other-reclassification-records huggingface dataset:
title: Contrasting Styles of Late Neogene Deep-Water Sandstone Depostition Offshore Texas
Creators: name: Morton, Robert A.
Publisher: name: The University of Texas at Austin
Year: 1990
Subjects: subject: stratigraphy
subject: depositional systems
subject: Neogene
subject: deepwater
subject: sandstone
subject: Texas offshore

description: Middle Miocene and middle Pliocene deep-water reservoirs of the western Gulf Coast Basin are associated with failed shelf margins and subregional unconformities referred to as submarine pediments. The submarine pediments formed broad, convex-landward arcs along nondeltaic slopes and on the southwestern flanks of subjacent delta systems. They were created by retrogressive failure and were later enlarged by erosion during periods of lowered sea level. At times of lowered sea level, the deep embayments carved into the continental platform funneled nearshore sands downslope to basin-floor fans. The pediments were first backfilled by deep-water mudstones deposited by mass transport processes. These slump blocks and high-energy turbidites exhibit mounded to chaotic seismic reflections that dip landward. Later, sand-rich channel-levee complexes were deposited above the basal mudstones and near the seismic fades transition from chaotic reflections to overlying horizontal or wavy reflections. The pre-entrenchment morphology of the shelf margin was finally restored by coalescence of small, prograding deltas that are recorded as clinoform reflections. Unconfined lower slope and basin-floor fans, associated with the submarine pediments, are generally sand-poor. The sand-rich lowstand fan deposits are restricted to highly elongate, dip-oriented leveed channels that mark the principal pathways of sediment transport. Sandstones confined to leveed channels of the upper fan and pediment fill are the most prolific hydrocarbon reservoirs within each stratigraphic sequence. These channel sandstones exhibit high vertical continuity but low lateral continuity because interbedded turbidite mudstones increase away from the channel axes. Thin sandstones of the lower fan may exhibit high lateral continuity, but they typically have poor reservoir properties because of high concentrations of original muddy matrix.
title: Hydrologic Characterization of Ground Water Resources in South Central Hudspeth County, Texas
Creators: name: Mullican, William F.
name: Senger, Rainer K.
Publisher: name: The University of Texas at Austin
Year: 1990
Subjects: subject: hydrology
subject: Hudspeth County
subject: Texas

description: Regional and local hydrologic investigations have been conducted in Trans-Pecos Texas at the principal study area for a low-level radioactive waste repository. The area is approximately 40 mi (65 km) southeast of El Paso in the Hueco Bolson, a fault-bounded desert basin that developed in the late Tertiary. Groundwater in the principal study area is found in Hueco Bolson silts and sands at depths of 361 ft (110 m) and 478 ft (146 m), and at depths of 592 ft (180 m) in Cretaceous limestones. The unsaturated zone consists of approximately 50 ft (15 m) of alluvial silt, sand, and gravel underlain by 300 to 500 ft (91 to 152 m) of lacustrine and fluvial clay, silt, and fine sand. The scope of this investigation included (1) evaluating groundwater resources in the area, (2) determining groundwater flow paths and velocities, and (3) testing hydrologic hypotheses using groundwater flow models. Development of groundwater resources in the vicinity of the principal study area is limited by two key factors: (1) costs of drilling and completing wells and of producing water at depths typically greater than 400 ft (122 m), and (2) the very low productivity of aquifers. Transmissivities of aquifers in bolson and Cretaceous strata, as revealed by 11 aquifer tests, range from approximately 0.19 to 290.0 ft²/d (0.018 to 26.9 m²/d); corresponding permeabilities range from 0.0015 to 2.82 ft/d (0.0005 to 0.861 m/d). A composite potentiometric surface based on water levels measured in all available wells and on the hydrologic interconnection of the Diablo Plateau aquifer, Hueco Bolson silt and sand aquifer, and Rio Grande alluvium aquifer indicates that groundwater is recharged on the Diablo Plateau and flows to the south and southwest toward the Rio Grande beneath the bolson pediment. The inferred distribution of permeability zones focuses flow from the eastern Diablo Plateau toward Cretaceous outcrops along the Campo Grande fault, creating an observed potentiometric high. The relatively low hydraulic heads near the principal study area are caused by preferential drainage along relatively permeable bolson deposits to the west and southwest toward the Rio Grande. Water chemistry data, particularly on tritium, carbon-14, and total dissolved solids, generally support the interpreted flow pattern; some discrepancies can be related to paleohydrologic effects associated with the incision of the Rio Grande during Quaternary time.
title: Consolidation of Geologic Studies of Geopressured-Geothermal Resources in Texas
Creators: name: Raney, J. A.
name: Seni, Steven J.
name: DuBar, Jules R.
name: Walter, T. G.
Publisher: name: The University of Texas at Austin
Year: 1991
Subjects: subject: geothermal energy
subject: geopressured zones
subject: Texas
subject: research

description: In a five-county area of South Texas, geopressured-geothermal reservoirs in the upper Wilcox Group are colocated with heavy-oil reservoirs in the overlying Jackson Group. In 1990, research at the Bureau of Economic Geology concentrated on evaluating the potential of using geopressured-geothermal water for hot-water flooding of heavy-oil reservoirs. Favorable geothermal reservoirs are defined by thick deltaic sandstones and growth-fault-bounded compartments. Potential geothermal reservoirs are present at a depth of 11,000 ft (3,350 m) to 15,000 ft (4,570 m) and contain water at temperatures of 350°F (177Â°C) to 383°F (195°C) in Fandango field, Zapata County. One potential geothermal reservoir sandstone in the upper Wilcox (R sandstone) is composed of a continuous sand body 100 ft (30 m) to greater than 200 ft (>61 m) thick. Fault blocks average 2 to 4 mi^2 (5.2 to 10.4 km^2) in area. Both heavy-oil (average API=19) and light-oil (average API=26) reservoirs in South Texas are present in sandstones of the Jackson Group Mirando trend. The updip pinch-out of strike-oriented sheet sandstones in the Jackson Group largely controls the distribution of Mirando-trend heavy-oil reservoirs. The lateral continuity of heavy-oil reservoirs minimizes reservoir compartmentalization, which could disrupt injected-fluid flow paths. Geologic and engineering research that still needs to be conducted includes (1) studies of the chemical compatibility between injected geothermal fluids and clay matrix of heavy-oil reservoirs, (2) detailed field studies of geometry and size of geothermal reservoirs, (3) detailed field studies of geometry and size of heavy-oil reservoirs, and (4) studies of changes in the temperature and chemistry of geothermal fluids when injected into heavy-oil reservoirs.
title: Structure, Facies, and Internal Properties of the Frio 'A' Reservoir, Hitchcock N. E. Field, Galveston County, Texas
Creators: name: Light, M. P. R.
Publisher: name: The University of Texas at Austin
Year: 1985
Subjects: subject: petroleum
subject: reservoirs
subject: Frio Formation
subject: Galveston County
subject: Texas

description: The N.E. Hitchcock field, which produces from the Frio 'A' or 9,100 ft sandstone, is defined by a northwest plunging anticline of moderate relief. It is truncated on its southeast flank by a major fault downthrown several hundred feet to the south. Several minor faults displace the original pay zone and may influence enhanced gas recovery efforts in the reservoir. The Frio 'A' sandstone, which occurs at the top of the Frio Formation in the Chocolate Bayou area, forms part of a constructive delta lobe in the N.E. Hitchcock field. It consists of a stacked sequence of distributary-mouth-bar sandstones which grade into a thin delta destructional unit and are overlain by the transgressive shallow-marine Anahuac shale. Marine reworking of the Frio 'A' sandstone has resulted in its broad lateral extent and internal continuity although thin shale breaks vertically partition the reservoir. Much of the preserved excellent porosity (≥ 30%) and permeability (≥ 1,000 md, 0.99 μm²) in the Frio 'A' sandstone is due to its distributary-mouth-bar origin. The porosity and permeability were subsequently modified by diagenetic reactions. The Frio 'A' aquifer extends some eight miles southwest of the N.E. Hitchcock field to the Alta Loma and Sarah White fields. It is confined on its northern and southern flanks by major growth faults. The continuity of the Frio 'A' sandstone has bearing on any plans to control water influx by drilling additional guard wells below the gas-water contact. However, reservoir modeling suggests that the faults are not sealing during co-production pressure drawdown. Variable areas of indurated authigenic kaolinite zones developed in the Frio 'A' sandstone adjacent to thin shale units probably result from fluids emitted from the shales which have a consistent illite-smectite composition. Slight reductions in salinity during production at the Prets No. 1 well may be evidence for contemporaneous dewatering of shales. Shale pyrolysis data indicate that the Anahuac and Frio shales are of too poor a quality and are too immature to have generated appreciable hydrocarbons. Furthermore, isotope data for the Prets No. 1 condensates imply a marine organic source for these fluids. Thermal and hydrocarbon maturity data indicate that the Upper Frio was subjected to an extended period of hot, extremely saline, basinal-fluid flow. This fluid flow appears to have introduced the hydrocarbons and caused albitization of feldspars and formation of carbonate cements.
Supplementary document for Fast interrogation of intestinal organ-on-chip devices through inverted single plane illumination microscopy (iSPIM) using an electro-tunable lens - 7455133.pdf
Creators: name: Manzano, Emilio Gualda
name: Abad-Lázaro, Aina
name: Altay, Gizem
name: Castro-Olvera, Gustavo
name: Bernardello, matteo
name: Fernández-Majada, Vanesa
name: Martínez, Elena
name: Loza-Alvarez, Pablo
Publisher: name: Optica Publishing Group
Year: 2025
Subjects: Biological Engineering

description: Suplementary Figures
Parastilobezzia Wirth & Blanton 1970
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Parastilobezzia

description: Genus Parastilobezzia Wirth & Blanton
Parastilobezzia Wirth & Blanton, 1970a: 10. Type species, Parastilobezzia leei Wirth & Blanton (orig. des.).
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 122, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
title: Consolidation of Geologic Studies of Geopressured-Geothermal Resources in Texas: Colocation of Heavy-Oil and Geothermal Resources in South Texas
Creators: name: Seni, Steven J.
name: Walter, T. G.
name: Raney, J. A.
Publisher: name: The University of Texas at Austin
Year: 1992
Subjects: subject: geothermal energy
subject: geopressured zones
subject: heavy oil
subject: Texas

description: In a five-county area of South Texas, geopressured-geothermal reservoirs in the Eocene Wilcox Group occur below heavy-oil reservoirs in the Eocene Jackson Group. This colocation warrants consideration of the use of geothermal fluids for a thermally enhanced waterflood. Geothermal fairways comprise thick deltaic sandstones within growth-fault-bounded compartments containing geopressured water in excess of 250°F. Geothermal reservoirs occur at depths of 11,000 to 15,000 ft in continuous sandstones 100 to 200 ft thick. Permeability ranges from 1 to 150 md, and porosity from 12 to 24 percent. Updip pinch-out of shallowly buried (200 to 2,000 ft) barrier-bar/strandplain sandstones largely controls the distribution of heavy-oil reservoirs. Subtle structure, small faults, and sandbody pinch-outs form lateral barriers of the reservoirs. Structural, depositional, and diagenetic variations affect reservoir compartmentalization. The heavy-oil reservoirs are typically porous (25 to 35 percent), permeable (100 to 1,000 md), slightly clayey fine to medium sand. Calcite-cemented zones of low porosity (>5 percent) and permeability (0.01 md) compartmentalize reservoirs. Injection of hot (300°F), moderately fresh to saline brines will improve oil recovery by lowering viscosity and decreasing residual oil saturation. Matrix clays are smectites, which could swell and clog pore throats if injected waters were fresh. The high temperature of injected fluids will collapse some of the interlayer clays, thus increasing porosity and permeability. Reservoir heterogeneity resulting from facies variation and diagenesis must be considered when siting production and injection wells within the heavy-oil reservoir. The suitability of abandoned gas wells as geothermal production wells and their long-term well productivity also affect the economics of geothermally enhanced hot-water flooding.
title: Radiocarbon Age of Quaternary Deposits, Western Rolling Plains of Texas
Creators: name: Caran, S. Christopher
name: Baumgardner, Robert W.
Publisher: name: The University of Texas at Austin
Year: 1985
Subjects: subject: Quaternary
subject: geochronology
subject: radiocarbon dating
subject: Texas

description: Four laboratories have made more than fifty finite radiocarbon-age determinations on samples from Quaternary deposits covering a large area of the Rolling Plains. These dates span the period from the late Pleistocene Epoch (23,255 ± 2,335 yr B.P.) virtually to the present. Caran and Baumgardner (1984) described a previously unrecognized sedimentary sequence covering more than 7,800 km2 (3,000 mi2) of northwestern Texas. At the time that report was prepared, only a few relevant radiocarbon-age determinations were available. The number of reliable finite dates has now increased to more than fifty, the oldest of which is 23,255 ± 2,335 yr B.P. Older infinite dates and a few questionable finite determinations also have been obtained, some of which were reported previously by other investigators.
title: Geology and Hydrology of the Northern Segment of the Edwards Aquifer with An Emphasis on the Recharge Zone in the Geogetown, Texas, Area
Creators: name: Kreitler, Charles W.
name: Senger, Rainer K.
name: Collins, Edward W.
Publisher: name: The University of Texas at Austin
Year: 1987
Subjects: subject: groundwater
subject: Edwards Aquifer
subject: recharge
subject: Georgetown
subject: Texas

description: In March 1986, the Bureau of Economic Geology was contracted by the Texas Water Development Board to conduct geologic and hydrologic investigations of the northern segment of the Edwards aquifer along the Balcones Fault System in the Georgetown-Round Rock area, particularly to elucidate the processes and areas of recharge for the Edwards in the Georgetown area. Geological mapping, combined with analysis of fractures in Comanche Peak, Edwards, and Georgetown limestones (Edwards aquifer strata) in the vicinity of Georgetown and Round Rock, Texas, was conducted to provide data useful in identifying potential recharge areas, assessing local groundwater flow, and enhancing our understanding of the geology of the Balcones Fault Zone. Cretaceous Comanche Peak, Edwards, Georgetown, Del Rio, Buda, Eagle Ford, and Austin strata dip gently (1°) eastward and are overlain in some places by terrace deposits and alluvium. Several major normal faults, downthrown to the east, strike northward across the area. Gentle flexures, possibly related to faulting, parallel the faults. Minor normal faults and joints are most abundant in areas adjacent to major faults and flexures. These fractured-strata zones likely parallel the length of the faults or flexure axes and may be as wide as 1.6 km. Most minor faults strike between 340°-040°, have displacements less than 2 m, and dip from 40°-80° both eastward and westward. Most joints strike between 340°-020° and 260°-300°, and fracture densities range from 4 joints per meter to 1 joint per 5 meters in 1 to 2-meter-thick beds.
title: The Artesia Group and Salado Formation (Guadalupian/Ochoan) of Palo Duro Basin: Depositional Systems and Effects of Post-Permian Salt Dissolution
Creators: name: Nance, Hardie Seay, 1948-
Publisher: name: The University of Texas at Austin
Year: 1987
Subjects: subject: stratigraphy
subject: depositional systems
subject: Permian
subject: salt dissolution
subject: Palo Duro Basin

description: Interbedded red sandstone, siltstone, mudstone, anhydrite, and halite make up the Artesia Group and Salado Formation (Guadalupian/Ochoan) of the Palo Duro Basin. These deposits accumulated in a 10,000-mile2 low-relief epicontinental basin characterized by regional aridity and episodic, nearly basin-wide influx of marine-derived hypersaline waters. Various depositional environments developed, including eolian dunes, interdune areas, eolian flats, intermittent fluvial, mud flats, and broad, shallow brine pans. Clastic sources were in the west and northwest, while evaporites were derived from the south. Eolian dune deposits exhibit medium to high angle (15°-35°) cross-bedded fine sandstone. Interdune areas accumulated rippled, bimodal, medium to very fine sandstone with frosted, spherical, medium sand grains and pedogenic structures. Eolian flats are characterized by deposits of very fine sandstone with poorly defined ripples. Intermittent fluvial deposition resulted in very fine sandstones and siltstones with graded bedding, ripples with mud drapes, and intraclasts. Mud-flat deposition produced mudstones with very disturbed ripples. Bedded halite and anhydrite precipitated in brine pan environments. Landward margins of brine pans feature deposits of sandstone and siltstone with displacive halite to chaotic halite-mudstone rock. Artesia and Salado facies occur in a characteristic vertical sequence that comprises, from base to top, bedded anhydrite, bedded halite, chaotic halite-mudstone, sandstone, and siltstone with displacive halite, very disturbed rippled mudstone, intermittent fluvial, and eolian elastics. The sharp contacts between these shallowing-upward sequences suggest rapid transgressions. Subsequent to upper Permian deposition, undetermined amounts of halite strata have been removed by dissolution, resulting in truncation of halite beds and collapse and diagenetic alteration in overlying strata.
Tephritis praecox
Creators: name: Kovac, D.
name: Kameneva, E. P.
name: Korneyev, V. A.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Tephritidae
Tephritis
Tephritis praecox

description: Tephritis praecox (Loew, 1844)
Strobl, 1904: 559 — Zara; Bjeliš, 2007: 373.
Remarks. Not represented in our material. Larvae infest flower heads of Calendula arvensis (Asteraceae) (Merz, 1994).
description: Published as part of Kovac, D., Kameneva, E. P. & Korneyev, V. A., 2022, A Review Of Tephritidae And Ulidiidae (Diptera, Tephritoidea) Of Croatia, pp. 349-372 in Zoodiversity 56 (5) on page 358, DOI: 10.15407/zoo2022.05.349, http://zenodo.org/record/7427863
Parastilobezzia leei Wirth & Blanton 1970
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Parastilobezzia
Parastilobezzia leei

description: leei Wirth & Blanton, 1970a: 10. Type locality: Colombia, Valle del Cauca (Río Raposo). HT F (# 70651 USNM). Distr.: Costa Rica, Colombia (Valle del Cauca (Río Raposo)). Refs.: Wirth & Blanton, 1970a: 12; Borkent & Spinelli, 2007: 84; Borkent, 2015: 132 (cat.).
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 122, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
title: Hydrogeology and Hydrochemistry of the Ogallala Aquifer, Southern High Plains
Creators: name: Nativ, Ronit
Publisher: name: The University of Texas at Austin
Year: 1987
Subjects: subject: aquifers
subject: Ogallala Aquifer
subject: High Plains

description: The Ogallala aquifer, which underlies the Southern High Plains, consists of the saturated sediments of the Ogallala Formation (Neogene). It serves as the main source of water for the High Plains of Texas and New Mexico but has been severely depleted due to extensive pumpage. The hydrology and hydrochemistry of the aquifer are influenced by the surface topography of the underlying formations and the thickness and permeability of formation deposits. Two distinct hydrogeologic provinces were observed. The first province, located along paleo valleys filled with coarse fluvial sediments, exhibits increased formation thickness and saturated section, as well as higher porosities and hydraulic conductivities. Ground-water flow lines within this province follow the orientation of the paleo valleys. The hydrochemical composition in this province remains relatively constant, characterized by Ca-HCO3 to mixed-HCO3 water, depleted in 0180, δD, and tritium. In contrast, the second hydrogeologic province features thinner and less permeable formations, primarily composed of fine-grained eolian elastics. Ground-water discharge from aquifers in the Cretaceous contributes to the hydrochemical facies, resulting in isotopic compositions different from those of the first province. Cross-formational movement of water and low permeability in the Ogallala Formation in these areas lead to varying hydrochemical facies and isotopic compositions. Secondary factors influencing the chemical composition of Ogallala Formation ground water include contamination from evaporating saline lakes, agricultural chemicals and fertilizers, and oil field brines. The impact of these chemicals may increase in the future as contaminants continue to move through the unsaturated zone toward the water table.
Stilobezzia Kieffer 1911
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Stilobezzia

description: Genus Stilobezzia Kieffer
Stilobezzia Kieffer, 1911a: 118. Type species, Stilobezzia festiva Kieffer (orig. des.). Refs.: Huerta, 1996 (key to males and females from Mexico); Ingram &Macfie, 1931 (key males and females from Patagonia and southern Chile); Lane & Forattini, 1961 (key to males and females from Neotropical Region north of Patagonia and southern Chile); Wirth & Grogan, 1988 (key to subgenera, as part of generic key).
Hartomyia Malloch, 1915a: 339. Type species, Ceratopogon pictus Coquillett (= Stilobezzia coquilletti Kieffer) (orig. des.).
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 122, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
title: Fracture Analyses of the Palo Duro Basin Area, Texas Panhandle and Eastern New Mexico
Creators: name: Collins, Edward W.
name: Luneau, Barbara A.
Publisher: name: The University of Texas at Austin
Year: 1985
Subjects: subject: fractures
subject: tectonics
subject: Texas Panhandle
subject: New Mexico
subject: Palo Duro Basin

description: Fracture analyses of the Palo Duro Basin area, Texas Panhandle, and Eastern New Mexico provide clues to the structural history of the area and help to determine the occurrence and characteristics of the fractures and veins in strata of this region. Fractures are associated with folds and faults that occur along the margins of the basin as well as in relatively undeformed strata within the central basin area. Along the Amarillo Uplift, the strikes of fractures in Permian and Triassic rocks are different from fracture orientations in overlying Tertiary strata. Fracture orientations determined by fracture identification logs from wells in Deaf Smith and Swisher Counties indicate similar fracture strikes in Pennsylvanian and Permian strata within the basin. Throughout the region, fractures that strike east-west (275°-295°) and northwest-southeast (305°-320°) are the most common. Zones of closely spaced fractures occur in outcropping Permian and Triassic strata. The width of the joint zones may be as great as 40 m, and the zones may extend laterally for distances of up to 0.75 km or possibly farther. Gypsum veins are common in strata that have undergone collapse following salt dissolution, whereas halite veins commonly cut salt-bearing strata. Even though a subpolygonal pattern on bedding planes suggests a synsedimentary origin for some of the halite veins, a variety of cross-cutting relationships also indicate post-compactional origins for many of the halite veins.
title: Relationship Between Radar Lineaments, Geologic Structure and in Situ Stress in East Texas
Creators: name: Baumgardner, Robert W.
Publisher: name: The University of Texas at Austin
Year: 1988
Subjects: subject: radar
subject: geology
subject: structure
subject: stress
subject: East Texas

description: Radar-based lineaments in East Texas and northwest Louisiana were studied to determine their relationship to surficial and subsurface geologic structure and to in situ stress. For all lineament data, two significant azimuths of vector sums were defined: 325° and 37°. The northwest trend has the same orientation as the mean direction of wellbore elongations in the Schuler Formation throughout the East Texas Basin. However, this trend is significantly different from the 344° orientation of wellbore elongation in the overlying Travis Peak Formation. These results suggest a complex relationship between subsurface stress and the northwest lineament trend. The northeast lineament trend does not coincide with the orientation of any known stress or regional structure and may be an artifact of radar illumination direction. Unlike a previous regional study based on smaller-scale Landsat data, no consistent correlation between surficial or subsurface structure and lineament density was discovered. However, high values of lineament density occur preferentially on outcrops of the Sparta and Leeches Formations. These results suggest that either most radar lineaments smaller than Landsat lineaments are manifestations of unmapped subregional or local structures or most radar lineaments are surficial phenomena, unrelated either to subsurface geologic structure or to stress.
Tephritis ruralis
Creators: name: Kovac, D.
name: Kameneva, E. P.
name: Korneyev, V. A.
Publisher: name: Zenodo
Year: 2022
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Tephritidae
Tephritis
Tephritis ruralis

description: Tephritis ruralis (Loew, 1844)
Langhoffer, 1928.
Remarks. Not represented in our material. Larvae infest flower heads of Hieracium pilosella and H. lactuella (Asteraceae) (Merz, 1994).
description: Published as part of Kovac, D., Kameneva, E. P. & Korneyev, V. A., 2022, A Review Of Tephritidae And Ulidiidae (Diptera, Tephritoidea) Of Croatia, pp. 349-372 in Zoodiversity 56 (5) on page 359, DOI: 10.15407/zoo2022.05.349, http://zenodo.org/record/7427863
title: An Assessment of the Natural Gas Resource Base of the United States
Creators: name: Fisher, W. L. (William Lawrence), 1932-
name: Finley, Robert J.
name: Seni, Steven J.
name: Ruppel, Stephen C.
name: White, William Allen, 1939-
name: Ayers, W. B.
name: Dutton, Shirley P.
Publisher: name: The University of Texas at Austin
Year: 1988
Subjects: subject: resources
subject: assessment
subject: United States

description: The distribution of natural gas in the United States comprises proved reserves in known reservoirs, inferred reserves, undeveloped resources within these reservoirs, and undiscovered resources. Beyond proved reserves, all volumes of future natural gas supply are estimates based on information derived from past and current experience in gas production and reservoir development. Even proved reserves are subject to periodic revision. This assessment begins with an understanding of major components of the natural gas supply derived from existing resource estimates that use established methodologies. In addition to historically defined elements of the resource base, a new component—reserve growth in heterogeneous reservoirs—is quantified in this study. Resource assessments proceed in their planning and compilation from reasonably well-known quantities (proved reserves) to increasingly less well-known quantities (undiscovered resources). Furthermore, natural gas reservoirs termed unconventional are typically given separate consideration and include gas in low-permeability reservoirs, gas in shale formations such as the Devonian of the Eastern U.S., and coalbed methane resources. This approach has been followed in this assessment. Special note was made of Alaskan gas reserves as they are significant and proven, but transportation for North Slope gas to the Lower 48 states is lacking.
title: Description and Quaternary History of the Campo Grande Fault of the Hueco Basin, Hudspeth and El Paso Counties, Trans-Pecos Texas
Creators: name: Collins, Edward W.
name: Raney, J. A.
Publisher: name: The University of Texas at Austin
Year: 1989
Subjects: subject: faults
subject: Quaternary
subject: Campo Grande Fault
subject: Hueco Basin
subject: Trans-Pecos Texas

description: The Hueco Basin of Trans-Pecos Texas and Chihuahua, Mexico, formed in response to Basin and Range extensional tectonism that began about 24 million years ago and continues to the present. The southeastern arm of the basin is asymmetrical, with the thickest sediments deposited along the fault-bounded basin axis near the southwestern flank. Approximately 45 kilometers long and striking northwestward, the Campo Grande fault is 12 kilometers from the northeastern basin edge; it divides the downthrown central part of the basin (with over 2,000 meters of fill) from the shallower (175 meters) northeastern flank. Another major northwest-striking fault dips northeastward and bounds the southwestern basin margin in Mexico. The Campo Grande fault trend is composed of at least 17 en echelon fault strands that are 1.5 to 10 kilometers long, with strikes of N25° to 75°W. Dips range between 60 and 90° southwest. Displacements decrease near the terminations of strands. Grooves on fault planes indicate mostly dip-slip movement. Fault scarps have been modified by erosion of the footwall and deposition on the hanging wall. Erosion-resistant caliche (stages IV to V) at the surface aids in preserving scarp heights ranging from 1.5 to 11.5 meters and scarp slopes of 4 to 17°.
Acanthohelea Kieffer 1917
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Acanthohelea

description: Subgenus Acanthohelea Kieffer
Acanthohelea Kieffer, 1917a: 198. Type species, Acanthohelea pruinosa Kieffer (mon.).
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 122, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
Acanthohelea maia Lane & Forattini 1958
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Acanthohelea
Acanthohelea maia

description: maia Lane & Forattini, 1958: 204. Type locality: Panama, Prov. Panamá, Almirante, Bocas del Toro. HT M (DEFS). Distr.: Panama, Colombia (?). Refs.: Lane & Forattini, 1958: 204; Borkent & Spinelli, 2007: 85.
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 123, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
Clinohelea Kieffer 1917
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Clinohelea

description: Genus Clinohelea Kieffer
Clinohelea Kieffer, 1917b: 295. Type species, Ceratopogon variegatus Winnertz (= Ceratopogon unimaculata Macquart) (orig. des.).
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 123, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
title: Child’s Rights oriented Teaching and Learning
Creators: name: Conrad, Sarah-Jane
name: Schmid Giacomini, Corinne
name: Burato, Martina
name: Fiechter, Ursula
name: Gubler, Moritz
name: Heierle, Daniela
name: Kipfer, Dunja
name: Koch, Eva
Publisher: name: :unas
Year: 2024

description: The poster highlights the integration of the United Nations Convention on the Rights of the Child (UNCRC) into teacher education at the University of Teacher Education Bern. This initiative responds to critiques from the UN Committee regarding insufficient knowledge of the UNCRC among professionals in Switzerland, limiting its transformative potential in education. Funded as part of an innovation project, the aim was to embed children’s rights systematically into teacher training across primary, secondary, special needs, and continuous education programs. The approach followed a step-by-step strategy, starting with identifying connections between the UNCRC and teacher education modules. Using the Whole Institution Approach, the project embedded children's rights into modules covering curriculum learning, social sciences, music, and migration. The UNCRC principles were made accessible by focusing on its general principles and models like Lundy’s framework for participation. Recurring references to the UNCRC in professional practice established it as a practical tool for rights-respecting learning environments. Findings demonstrated the positive impact of this embedded approach on teacher education. It reshaped students’ perceptions of children as rights holders, fostering a deeper understanding of inclusive, differentiated teaching. The integration also improved teacher competencies, enabling better support for diverse learners.
Ceratobezzia Kieffer 1917
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Ceratobezzia

description: Subgenus Ceratobezzia Kieffer
Ceratobezzia Kieffer, 1917b: 326. Type species, Ceratobezzia fallax Kieffer (orig. des.).
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 123, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
Ceratobezzia fallax Kieffer 1917
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Ceratobezzia
Ceratobezzia fallax

description: fallax Kieffer, 1917b: 326. Type locality: Paraguay. T F (HNHM, lost). Distr.: El Salvador to Colombia (Meta (Indostán)), Venezuela, Brazil (Amazonas, Pará, Mato Grosso, Sãom Paulo), Paraguay, Northeastern Argentina. Refs.: Kieffer, 1917b: 326; Spinelli & Duret, 1993: 41; Borkent & Spinelli, 2007: 88.
barrettoi Lane & Duret, 1954: 249. Type locality: Brazil, São Paulo, Ribeirao Preto. HT F (# 10433 DEFS).
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 123, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
Clinohelea Kieffer 1917
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Clinohelea

description: Subgenus Clinohelea Kieffer
Refs.: Spinelli & Duret, 1993 (key to males and females).
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 123, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
Clinohelea horacioi Lane 1944
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Clinohelea
Clinohelea horacioi

description: horacioi Lane, 1944: 257. Type locality: Brazil, São Paulo, São Roque. HT F (# 4984 DEFS). Distr.: Mexico (Yucatán, Tabasco, Morelos) to northeastern Argentina. Localities in Colombia (Valle del Cauca (Río Raposo), Meta (Indostán), Chocó (Vuelta)). Refs.: Lane, 1944: 257; Spinelli & Duret, 1993: 45; Borkent & Spinelli, 2007: 88.
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 123, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
title: Poinsettie, Weihnachtsstern :
title: Richtlinien für die Durchführung der Prüfung auf Unterscheidbarkeit, Homogenität und Beständigkeit.
titleType: Subtitle
Creators: name: (:Unas)
Publisher: name: Unknown
Year: 2008

description: Zweck dieser Richtlinien („Prüfungsrichtlinien“) ist es, die in der Allgemeinen Einführung (Dokument TG/1/3) und deren verbundenen TGP-Dokumenten enthaltenen Grundsätze in detaillierte praktische Anleitung für die harmonisierte Prüfung der Unterscheidbarkeit, der Homogenität und der Beständigkeit (DUS) umzusetzen und insbesondere geeignete Merkmale für die DUS-Prüfung und die Erstellung harmonisierter Sortenbeschreibungen auszuweisen.
title: Violences fondées sur le genre et intersectionnalité : de la théorie à l’action publique (LIEPP Policy Brief, n°69)
Creators: name: Lieber, Marylène
Publisher: name: Sciences Po - LIEPP
Year: 2023
Subjects: classificationCode: 5
subject: FOS: Social sciences

description: Quels sont les apports de près de 40 ans de recherche sur les violences fondées sur le genre et comment peut­-on les mobiliser pour l’action publique ? En retraçant les différentes théorisations effectuées par les recherches féministes sur les violences masculines envers les femmes ou fondées sur le genre, puis les critiques qui ont pu être adressées aux approches qui ne prennent pas en compte les expériences des populations minoritaires et minorisées, cet article entend attirer l’attention sur certains des enjeux théoriques et pratiques actuels, en présentant en particulier l’exemple de la lutte contre le « harcèlement de rue » sur laquelle l’autrice travaille depuis près de 20 ans.
Pellucidomyia Macfie 1939
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Pellucidomyia

description: Genus Pellucidomyia Macfie
Pellucidomyia Macfie, 1939a: 99. Type species, Pellucidomyia ugandae Macfie (orig. des.). Refs.: Wirth, 1960 (World key to males and females).
Macfiehelea Lane, 1946: 208. Type species, Macfiehelea oliveirai Lane (orig. des.).
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on pages 123-124, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
ПЕРСПЕКТИВЫ ИСПОЛЬЗОВАНИЯ АЛЬТЕРНАТИВНОГО ТОПЛИВА В ДВИГАТЕЛЯХ ВНУТРЕННЕГО СГОРАНИЯ СЕЛЬСКОХОЗЯЙСТВЕННОЙ ТЕХНИКИ
Creators: name: С.В. Михайлов
name: В.А. Седнин
Publisher: name: Zenodo
Year: 2024

description: В статье рассмотрены различные виды альтернативных моторных топлив. Приведены основные достоинства и недостатки отдельных видов альтернативных источников энергии, обозначены области их применения. Также рассмотрены различные модели тракторов, использующие альтернативное топливо. Даны основные оценки техническим проблемам при переводе сельскохозяйственной техники на альтернативные источники топлива. Сделан вывод о целесообразности перевода автотракторной техники для работы на альтернативных источниках энергии.
Pellucidomyia lanei Wirth & Ratanaworabhan 1971
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Pellucidomyia
Pellucidomyia lanei

description: lanei Wirth & Ratanaworabhan, 1971: 446. Type locality: Colombia, Valle del Cauca (Río Raposo). HT F (# 70678 USNM). Distr.: Colombia (Valle del Cauca (Río Raposo)), Jamaica. Refs.: Wirth & Ratanaworabhan, 1971: 446; Borkent & Spinelli, 2007: 89; Borkent, 2015: 145 (cat.).
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 124, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
title: A new approach to nutrient pollution governance in France and the EU (LIEPP Policy Brief, n°70)
Creators: name: Kanter, David
Publisher: name: Sciences Po - LIEPP
Year: 2023
Subjects: classificationCode: 5
subject: FOS: Social sciences

description: Nutrient pollution is a major environmental threat, fueled by synthetic fertilizer and manure use. However, the narrow focus of most policy on changing farmer behavior ignores the underlying forces that constrain their behavior. The "Governing Nutrient Pollution Beyond Farmers" project aims to build the scientific foundation for a new governance framework, centered around all the major actors in the agrifood system-from fertilizer manufacturers to supermarkets. This policy brief introduces the first proof of concept of this new approach, developed in collaboration with the Sciences Po Law Clinic and focused on the "algues vertes" problem in Brittany, which resulted in nine new policy proposals to address this seemingly intractable problem that span the entire agrifood system.
description: La pollution par les nutriments est une menace environnementale majeure, alimentée par l'utilisation d'engrais synthétiques et de fumier. Pour y pallier, la plupart des politiques publiques se concentrent sur le changement de comportement des agriculteurs et ne tiennent pas compte des réalités sousjacentes qui contraignent leur comportement. Le projet "Governing Nutrient Pollution Beyond Farmers" vise à établir les fondements scientifiques d'un nouveau cadre de gouvernance, centré sur tous les acteurs du système agroalimentaire, des fabricants d'engrais aux supermarchés. Ce Policy Brief propose une première présentation de cette approche novatrice, développée en collaboration avec la Clinique de l'Ecole de droit de Sciences Po et centrée sur la problématique des "algues vertes" en Bretagne. Celle­ci permet d'identifier neuf nouvelles propositions de politiques publiques pour résoudre un problème réputé insoluble qui touche l'ensemble du système agro­alimentaire.
TRANSFORMING EDUCATION: ASSESSING LEARNING  ENVIRONMENTS IN PUBLIC SCHOOLS WITH UEI-PDP
Creators: name: Amina Yasmeen, Qureshi
Publisher: name: TOP Journal
Year: 2024
Subjects: Quality, monitoring, positive change, professional development.

description: A positive change in the learning environment in schools is visible through ongoing professional development of teachers and administrators. Monitoring the professional development program and providing support to teachers and administrators to transfer their learnings into the school environment ensures some measures of quality. Quality issues led to the launching of the Professional Development Program (PDP) for Primary School Teachers (PSTs) of Sindh by the United Educational Initiative (UEI), a consortium of five Governmental and Non-Governmental Organizations, working under the supervision of Education Sector Reform Assistance (ESRA). Implementation of the UEI-PDP in four districts of Sindh, is ensured by a team of professionals in each district. Recognising that capacity building of district education employees would improve the educational system in the country, 130 Master Trainers were selected, on merit, from the District Education Office for the training of 17,000 teachers and 3000 Head teachers/administrators over a period of two years. This paper developed the design of a Monitoring Process for a Professional Development Program for Primary School Teachers and Administrators. Data was collected through Pre/Post-observations, Interviews, Questionnaires and Reports. Such tools make it possible for the monitoring teams to observe, to inquire further, and, along with the Managers, Master Trainers and School Support Team, seek to explain the progress of the program and take corrective action where indicated. Both formative evaluations as well as summative evaluation techniques are utilized for evaluating the program. The monitoring process that assisted in formative evaluations is described. In order to assist in summative evaluation, data collected through the monitoring process was further developed to categorize the schools where teachers and head teachers are trained. It is hoped that the categorization of the schools may lead to further improvements in those schools which fall in the group for need improvement. It may also initiate further research as to reasons behind why some schools are in the good category and why others fall in the average category.
Culicoides wirthi  1956
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Culicoides
Culicoides wirthi

description: wirthi (Lane), 1956b: 437 (Macfiehelea). Type locality: Panama, Canal Zone, Mindi Dairy. HT F (USNM). Distr.: USA (Texas) to Colombia (Meta (Finca Barbascal)). Refs.: Lane, 1956b: 437; Wirth & Ratanaworabhan, 1971b: 446; Borkent & Spinelli, 2007: 89.
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 124, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
Forcipomyia muzoni Spinelli & Duret 1993
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Forcipomyia
Forcipomyia muzoni

description: muzoni Spinelli & Duret, 1993: 46. Type locality: Colombia, Valle del Cauca (Río Raposo). HT F (USNM). Distr.: Colombia (Valle del Cauca (Río Raposo), Chocó (Río Sucio)). Refs.: Spinelli & Duret, 1993: 46; Borkent & Spinelli, 2007: 88; Borkent, 2015: 143 (cat.).
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 123, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311
title: Improving Accessibility at Nichols Arboretum
Creators: name: Farber, Taryn
name: Gallagher, Maia
name: Guo, Yingxue
name: Li, Jinbo
Publisher: name: University of Michigan
Year: 2024
Subjects: subject: trails
subject: accessibility
subject: mobility
subject: agroecology

description: Matthaei Botanical Gardens and Nichols Arboretum (MBGNA) is committed to fostering equitable and just access to the outdoors for everyone via its trail system and varied ecosystems. Currently, outdoor experiential inequities at Nichols Arboretum (the Arboretum) affect individuals with physical disabilities and limitations. While there are countless measures that would improve inclusion for people with all marginalized identities, time and capacity limitations required us to emphasize the ways in which Nichols Arboretum can reduce experiential inequities for visitors with physical disabilities specifically. Thus, there is always room to be more inclusive, but our efforts are meaningful steps towards equitable inclusion, which stakeholders have received enthusiastically. Moreover, our final suggestions include some ideas to broaden inclusion for other marginalized identities. After preliminary precedent studies and analyses of similar sites, we focused our analytical efforts on the landscape dimensions of the
Lanehelea Wirth & Blanton 1972
Creators: name: Spinelli, Gustavo
name: Wolff, Marta
Publisher: name: Zenodo
Year: 2016
Subjects: Biodiversity
Taxonomy
Animalia
Arthropoda
Insecta
Diptera
Ceratopogonidae
Lanehelea

description: Genus Lanehelea Wirth & Blanton
Lanehelea Wirth & Blanton, 1972: 433. Type species, Lanehelea leei Wirth and Blanton (orig. des.).
description: Published as part of Spinelli, Gustavo & Wolff, Marta, 2016, FAMILY CERATOPOGONIDAE, pp. 98-141 in Zootaxa 4122 (1) on page 124, DOI: 10.11646/zootaxa.4122.1.15, http://zenodo.org/record/256311