bluuebunny/crossref_metadata_2025_split huggingface dataset:
Measurement Research on Influential Effect of Standardization on Technological Innovation
Authors: Liu Hui 
Published: July 2020

Abstract
There is a close relationship between standardization and technological innovation. Based on the analysis of the function mechanism of standardization on technological innovation, this paper has established measurement indexes of the influential effect of standardization on technological innovation. As structural equation modeling (SEM) has its own advantages over statistical methods such as correlation analysis, regression analysis and path analysis, this study attempts to measure the influence degree of standardization on technological innovation by adopting SEM method, and has established a measurement model and a structural equation model for the standardized technological innovation effect. In addition, the study has discussed the fuzzy DEA method to analyze the standardized technological innovation effect of DMUs, established the fuzzy DEA-based index system for evaluating standardized technological innovation effect, constructed the fuzzy DEA model for evaluating standardized technological innovation effect, and provided the solution process of the model.
Airportlization: The Inevitable Choice of the Integration and Innovation of the exhibition Industry in the Age of Traffic Economy——Practical observation in China
Authors: Li Tiecheng , Liu Li , Wu Namei 
Published: July 2020

Abstract
The Internet revolution has had a significant impact on the global economy and society. Human beings are moving from the industrial age to information civilization. As one of the representatives of the new economic form in information civilization, the flow economy will become a new economic development model. Both the exhibition economy and the airport economy have the attributes of flow economy, and both of them are developing rapidly in China. They both are in a state of integration and development. The integration of exhibition economy and airport economy is based on the functional synergy of industrial chain integration, and the spatial integration of urban exhibition clusters and airport economic zones. Based on the theory of industrial chain integration, industrial integration and economic symbiosis, this paper puts forward the concept of the integration of exhibition economy and airport economy. We try to construct functional synergy model and spatial integration model, and propose the mechanism of industry chain sharing, co-governance and symbiosis and comprehensive cost-oriented mechanism. Finally, suggestions were made on the location selection of the airport exhibition industry, the exhibition industry and the airport industry linkage, and the regional competition and cooperation of the airport exhibition industry.
Marine influence during deposition of the Kiliranjao Brown Shale, Central Sumatra, from palynology point of view
Authors: Fakhruddin R , Gumilar I S , Ramli T 
Published: July 2020

Abstract
The Eocene to Oligocene succession of the Kiliranjao Brown Shale was deposited in a lacustrine environment. This study combines palynological analysis and XRD analysis technique to investigate the possibility of marine influence during deposition of Kiliranjao lacustrine shale. Two biostratigraphic zonations of Karbindo section are Middle to Late Eocene Proxapertites operculatus Zone and Oligocene Meyeripollis naharkotensis Zone. The marine flooding surface, as shown by the peak of the abundance of mangrove pollen, is used to delineate the section into five parasequences. The tripartite stratigraphic architecture of Karbindo section is consists of early rift deposit (TS1), syn-rift deposit (TS2), and syn-rift deposit (TS3). Middle to Late Eocene coal and limestone facies (parasequence I) represents the TS1. Late Eocene to Oligocene parasequence II to IV (below MFS) shows the TS2 (deepening-upward lacustrine succession), and the shallowing-upward lacustrine succession of Oligocene parasequence V (above MFS) indicate the TS3. The abundance of mangrove and back mangrove palynomorph assemblages and the high amount of carbonate mineral from XRD analysis are the evidence of marine influence to the deposition of Karbindo section Brown Shale. The marine incursion to the lacustrine environment occurred from the adjacent nearby open sea, that separated by shoal area, which can submerge below sea level during a marine transgressive event. Marine incursion events did contribute to the deposition of Kiliranjao Brown Shale though further work is still needed.
Geological structure identification in Tulehu geothermal prospect area using gravity data analysis
Authors: Latuconsina N , Daud Y , Sulistyo A , Yunus F M , Kurniawan A 
Published: July 2020

Abstract
Tulehu is one of geothermal prospect areas located in east Indonesia, which is in Maluku Province. The geological condition of the area is dominated by quaternary volcanic rocks like lava flow, lava dome, and pyroclastic flow, which probably associated with Mt. Eriwakang and Mt. Huwe. But the area is mostly covered by limestone, especially in the southern part of the area. The geothermal prospect of Tulehu is indicated by the occurrence of hot springs spotted along Banda Fault, Banda-Hatuasa Fault, and Huwe Fault in the southern part of Tulehu. In order to understand the subsurface geological structure and its correlation to Tulehu geothermal system, gravity survey was conducted. Gravity survey was carried out using Scintrex CG-5 gravimeter with total of 130 stations were measured with 500 m spacing. The result of CBA and residual gravity indicated the existence of low gravity anomaly at the Mount Eriwakang, while the high gravity anomaly found around several structures obtained from Remote Sensing. Several structures were detected by FHD method, those are Huwe Fault, Banda Fault, Tulehu Fault, and Wayari Fault. Based on SVD method, the type of faults are identified. These structures also supported through 2-D gravity forward modeling. The 2-D gravity modeling results several layers that build the geothermal system of Tulehu, those are Limestone with density of 1.79 g/cc, Pyroclastic with density of 2.67 g/cc, Andesitic Lava with density of 2.6 g/cc, claycap with density of 2.2 g/cc, and Basement with density of 2.81 g/cc.
Estimation of suitable habitat and fishing ground for Leiognathus splendens (Cuvier, 1829) in Blanakan coast based on environmental and metal Zn parameters
Authors: Takarina N D , Pin T G 
Published: July 2020

Abstract
Blanakan coast is known as prominent fishing ground in West Java coastal ecosystems. This is related to the presence of suitable habitat for fish species living in coast. One of fish species known living in Blanakan coast and has commercial value is Leiognathus splendens. Respectively, this research aims to predict the suitable habitat for L. splendens by using environmental parameters including salinity, ph, dissolved oxygen (DO), temperature, turbidity and Zn. The habitat suitability estimation method used was the ranking and overlay of environmental parameters. Those parameters were combined and overlayed by using geographical information system assistance to identify the most suitable habitats. Based on the result, the most suitable habitats were located near river mouth. This habitat is influenced by high level DO (5.7 mg/L) and pH (7.51). Correspondingly, the suitable habitats near the river mouth considering that L. splendens has an adaptation to low salinity (9 ppt) and high turbidity (218.03 NTU) near river. In contrast, the less suitable habitats were identified offshore. In here, the habitats affected by high temperature (31 °C), Zn content (0.55 mg/L), low DO (1.1 mg/L) and pH (7.15). This research hence might contribute some potentially valuable insights into exploring the relationship between the L. splendens suitable habitats and the environmental parameters.
The development of forest fire monitoring and warning system for agroforestry areas in Uttaradit Province, Thailand
Authors: Homhuan S , Humhong C 
Published: July 2020

Abstract
Forest fire occurs regularly in the northern agroforestry of Thailand started in February to April and it causes economic and environmental losses. This study aimed to develop an automatic spatial data analysis system for monitoring and warning and a system for tracking and warning forest fires in agroforestry areas. Near real-time NDVI in dry season was analyzed to estimate the amount of biomass using a relationship between the NDVI and surveyed dataset. The biomass, hotspot, DEM, slope, aspect and relative humidity data were analyzed by Multi-criteria analysis (MCA) for forest fire risk area. The results are presented on web and mobile platform for forest fire warning. The estimated biomass of March was 7.5 to 9.1 tons/hectare, which corresponded with the results obtained from the field survey. The fire risk factors analysis including hotspot density, relative humidity, and landscape were used to produce the five risk levels. Each risk level area from one to five was 11.84 km2, 25.68 km2, 42.28 km2, 30.85 km2 and 20.65 km2, respectively. The forest fire monitoring and warning systems were designed and developed in open-source platform, which can be utilized for forest, fire monitor and warning for local administration as well as farmers in the area.
Hydrogeochemical model of Ciseeng geothermal field, Bogor, West Java
Authors: Ponka M A , Sahdaranr D N , Kurniadi D T , Yoga D A , Sihombing F M H , Supriyanto  
Published: July 2020

Abstract
Ciseeng geothermal field is located Northwest of West Java 40 km from Jakarta. Three surface manifestations are in Tirta Sayaga, Panjang Mountain, and Peyek Mountain. This study aims to build a hydrogeochemical model based on water analysis. The secondary regional geological data are retrieved to complete geological information of Ciseeng. The research method is divided into several stages: introduction includes the literature study, data collection includes the measurement of temperature and pH in several surface manifestations, rock sampling and structural geology analysis in Ciseeng. The type of manifestation that can be found in Ciseeng is a warm pool with chloride fluid type. Extensive travertine deposits were found in all three locations. The fluid temperature of three surface manifestations is about 30-38 °C with pH 6. According to the measurement of Na-K-Ca geothermometer, the reservoir temperature in Ciseeng geothermal field is 180 °C. The three manifestations of Ciseeng geothermal field are classified as mature water based on a ternary plot diagram. The isotopic analysis shows shifting in O18 indicating hydrothermal process due to magmatic activities in the subsurface. It is predicted that Ciseeng geothermal field is part of Salak/Pangrango Mountain geothermal system. The presence of surface manifestation confirms that geological structure trending from North to South, play a significant role to circulate the heated fluid in the subsurface and subsequently to the surface. The result is a geothermal conceptual model of Ciseeng field that shows the fluid origin and movement in the subsurface.
SEM-EDX study on authigenic clay minerals in sandstone of Jatiluhur formation
Authors: Astuti T R P , Aditiyo R , Oktavioni A , Supriyanto  
Published: July 2020

Abstract
The presence of authigenic clay minerals is usually found in sandstones where these minerals grow in the environment itself. Authigenic clay minerals provide benefits to sandstones, especially to determine the quality of porosity and permeability in sandstones. The samples in this study were collected from an outcrop of measured section at Cipamingkis’ River. The main goal of this study was to understand the presence of authigenic clay minerals in sandstones caused by the diagenetic process using Scanning Electron Microscope and Energy Dispersive X-Ray (SEM – EDX method. The results of this study were kaolinite, smectite, and illite found in very dominant amounts in sandstones as pore linings, pore fillings, replacement, and vug fillings.
Identification of accretionary wedge at Sumatra subduction zone using 2D seismic reflection
Authors: Risqi A N , Riyanto A , Hananto N D 
Published: July 2020

Abstract
This research is focusing on structure at Nias Islands subduction zone. Subduction zone Sumatra is the collision zone of Eurasia continental plate and Indo-Australia oceanic plate. Prior to the establishment of the subduction zone there is an event of the making of continental crust in which in this research area is marked by Wharton Fossil Ridge. An odd feature of the Sunda subduction zone is the non-volcanic forearc ridge that comes up raised sea level assemble a lot of islands betwixt the trench and the mainland. The forearc ridge is the cap of a chunky sequence of sediments and sections of sea floor, known as the accretionary wedge, that are folded, faulted and plastered into the upper plate. Accretionary wedge structure which has the melange rock characteristics because of the plates’ subduction, The accretionary wedge could be intrepred using seismic reflection data with characteristic reflector doesn’t formed or visible. The islands offshore southwestern Sumatra might have a akin origin. The most appropriate study of these is Nias, which its southwest coastline is 90 km form the subduction deformation front and 20 km above the dipping plate interface. Southwest of Nias, the oceanic seafloor is dipping at a homogeneous angle 6° to 7° against Nias for a horizontal distance of 25 km beneath the accretionary wedge, where it attaints a depth of just over 10 km. In this research it has been done 2D seismic reflection data processing and the interpretation of the Wharton fossil ridge establishment, subduction zone, and accretionary wedge.
Study on geochemistry of sea water intrusion effect in Jailolo geothermal system
Authors: Fortuna D A , Daud Y , Abidin Z 
Published: July 2020

Abstract
The possibility of seawater intrusion in geothermal systems is very likely to occur. This is caused by several locations of geothermal systems which are very close to the coast. This paper presents a geochemical analysis of the data manifestations of water and gas, to determine the effect of sea water on the Jailolo geothermal system. From the results of the water analysis, it is clear that the effect of sea water intrusion on the Jailolo geothermal system is shown in the anions and cations diagrams, which is almost all of the plots very close to the seawater points. So that the next analysis is focused on the position of mixing sea water with reservoir water and correction of the parameters that are affected by the mixing of sea water. It is intended that the resulting geochemical model can describe the actual reservoir conditions. If we did not include the correction factor to the calculation this will lead into mislead assessment of the reservoir temperature of geochemistry model which is the final result of the study/assessment. It is also necessary take into account for the next step of the process which is exploitation phase.
Characteristics of chromitite mineralization in Sebuku Island based on thin section, polished section, and geochemical data
Authors: Imani S N , Sihombing F M H , Indra T L , Nugraheni R D 
Published: July 2020

Abstract
Sebuku Island is located in Kotabaru Regency, South Kalimantan and is known as one of the main sources of laterite iron in Indonesia. Based on its tectonic setting, Sebuku Island is located within the suture zone that connects Southwest Borneo Block (SWB) and East Java West Sulawesi Block (EJWB). Due to its tectonic setting, Sebuku Island is composed of various rocks associated with suture zone, such as ophiolite rocks. The ophiolite rocks could host mineralization that occurred in Sebuku Island. The aim of this study is to determine the characteristics of lithology and mineralization as determinants of geological processes that influence the formation of rocks and mineral deposits in Sebuku Island. This study was carried out through petrological, petrographic, ore microscopy analysis, and geochemical analysis (x-ray fluorescence). 22 rock samples from Sebuku Island were collected and the result of this research shows that the chromite host rocks are composed of serpentinized dunite and serpentinite. Chromite minerals (FeCr2O4) were found in massive forms with cataclastic, brecciated texture and disseminated with pull-apart texture. Based on observation of the polished sections, it is known that the associated mineral of chromite is magnetite which is an alteration of chromite minerals. Chromitite chemical data shows the chromite composition is Al-rich (Cr# = 0.6) and classified as podiform chromitite formed by fractional crystallization. There are two magma series of igneous rock in the study area i.e. tholeiitic series consists of ultramafic-mafic rocks and calc-alkaline consists of micro-diorite. The abundance of Al2O3 and TiO2 in chromitite shows that Al-rich chromitite has formed in Supra Subduction Zone (SSZ) and has occurred near or above the Moho-transition zone.
Landslide susceptibility map of Bogor Area using analytical hierarchy process
Authors: Wicaksono Y S , Sihombing F M H , Indra T L 
Published: July 2020

Abstract
Landslide is one of the most common disaster in Bogor City and Bogor Regency. BNPB stated that between 2013–2018 there are 44 landslides with death toll of 68 persons. Therefore, it is important to generate map to identify landslide susceptibility in research area. In this study, we try to create landslide susceptibility map of Bogor area (Bogor Regency and Bogor City) using Analytical Hierarchy Process (AHP). We use various factors to identify landslide susceptibility, including slope curvature, slope gradient, topographic wetness index, slope aspect, elevation, stream power index, distance to river, river density, distance to lineament, lineament density, lithology type, soil type, normalized differential vegetation index, rain intensity, land cover, distance to road, and building density. Various factors above are derivative from openly accessed data of Digital Elevation Model (DEM), landslide distribution, Bakosurtanal Map, Landsat 8 Imagery, engineering geology map, rain intensity data, and soil type map. After all, input data collected, the landslide susceptibility map is created using the AHP method. To validate the result, Receiver Operating Characteristic (ROC) applied, the value of the area under the curve (AUC) to determine the success rate of the AHP method is 0.834, this value represents that the landslide suscepbility map produced by the AHP method is a good model.
Reservoir quality derived from routine core analysis data of deep-water turbidite outcrop analogue
Authors: Prasetio R B , Prasojo O A , Oktavioni A 
Published: July 2020

Abstract
Turbidity current is a process where the fluid flows occurs as a turbulent flow where the molecules inside the fluid are moving randomly but with a net movement toward the orientation of the transport. The physical properties of turbidite deposit is highly impacted by the grain size distribution and rock texture during the deposition. The field in this study was an outcrop of Jatiluhur Formation which deposited by turbidity current on deep marine environment. The main goal of this study was to understand the correlation between the petro-physical properties of turbidite deposit with its depositional mechanism using the routine core analysis method. The samples in this study were collected from an outcrop and the routine core analysis data contains the percentage value of porosity and vertical permeability. The result of this study were the porosity was relatively equal to the permeability and depositional mechanism had a significant role in controlling the porosity and the permeability.
Ichnofossil significance on paleogeographic reconstruction and deep water turbidite reservoir
Authors: Grandis G , Prasojo O A 
Published: July 2020

Abstract
Petro-physical properties are the most important factor that controls the quality of the reservoir. Porosity, permeability, and the grain size are the main parameters to measure the quality of the reservoir. Thin section analysis was used to identify the arrangement of the grains within the rock. The existence of trace fossil can change the condition of the parameters of the reservoir. Bioturbation trace in a rock which made by organism activity, Planolites, changes the quality of reservoir significantly. The porosity value in a bioturbated zone was around 80 % and in the non-bioturbated zone wais 5 %. It increased the permeability too. This was identified from the interconnected pores in the bioturbated section, it has 90 % of quartz mineral with the same grain size relatively in bioturbated section and non-bioturbated section. The existence of Planolites trace implied that the outcrop was deposited in the deep-marine environment.
Estimation of anisotropy parameters VTI (vertical transverse isotropy) using velocity variation with offset (VVO) method, case study: BS oil field
Authors: Simarmata K O E , Suroso T , Supriyanto  
Published: July 2020

Abstract
Implementation of anisotropy value in seismic data processing greatly affect seismic cross section image. In addition to enhanced seismic imagery, anisotropy can be used for identification of hydrocarbons. In this study, the vertical transverse isotropy (VTI) anisotropy parameter estimation by the VVO method has been done. The magnitude of the velocity value of the offset/angle is due to the ever-greater velocity with a large incidence angle being the basis of the VVO method to demonstrate the anisotropy effect. The residual moveout result of the time transfer correction caused by the velocity increase will be used as input data. Validity of the VVO method is tested using a synthetic forward modelling to obtain anisotropy parameters that describe the subsurface conditions of the target area which are then applied to the actual data. The results found that residual values continued to increase due to the anisotropy effect and there after the angle of 30 degrees with the value of ɛ = 0.14 and δ = 0.049.
Optimizing seismic attribute to unlock facies change at Eocene-Oligocene fluvial deltaic sandstones of Pematang formation: Case study the “M” field, Central Sumatera Basin
Authors: Karwin  , Haris A 
Published: July 2020

Abstract
The “M” Field is in the Northern most of the Oil Prolific Central Sumatera Basin at Barumun sub-Basin. The field was originally discovered by drilling M-1 well. This well became the first well proving up the presence of hydrocarbon at Pematang Formation in this region. Pematang Formation is unique because it can serve as reservoir rock as well as source rock. The MX reservoir is part of the Pematang Formation. Based on the last drilling data in which it flows 200 barrels of oil. However, the sand of this reservoir disappeared at the other well, even though the location is not too far. This paper addresses the strategic approaches to interpret facies change using Acoustic Impedance (AI) Inversion. The facies change is detected using AI. It is challenging reservoir since its individual thickness is below seismic resolution. Geologically the MX reservoir was deposited under fluvial deltaic lacustrine environment. The result shows that M-2 is in the delta front facies while the M-1 is in the pro-delta facies. Even though only 1.6 km distance between M-2 and M-1 well cause significant facies change. Result of this study is useful for determining development drilling program in this field.