cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.28917410
title: Petrological and Re-Os isotopic constraints on the origin of chromitites and peridotites of the late cretaceous Waziristan ophiolite, western Pakistan: implications for subduction initiation

description: The Waziristan Ophiolite Complex (WOC) occurs between the Afghan microplate in the west and the Indian plate in the east along the Main Waziristan Thrust in western Pakistan. A complete ophiolitic sequence, including residual lherzolites, harzburgites with foliated and discordant dunites, gabbroic rocks, dyke swarms, pillow and massive basaltic rocks, is present in the complex. Widespread podiform chromitites are usually enclosed by thin dunitic haloes in the complex. Chromian spinels in lherzolites-harzburgites are characterized by Cr# [= Cr/(Cr  +  Al)] values ranging from 0.19 to 0.60, and plot within or overlap the fields of abyssal to fore-arc peridotites, while chromian spinels in dunites and chromitites with Cr# values from 0.57 to 0.79 exhibit geochemical affinities similar to those of boninites. Trace element and REE characteristics, including the enrichment of light REE in the Waziristan Complex peridotites indicate the contribution of subduction-related fluids/melts, including boninitic mantle melts, validating a subduction initiation process in their genesis, and these features are similar to those observed in supra-subduction zone peridotites. Chromitites are characterized by enrichment of Os, Ir, Ru and Rh relative to Pt and Pd on a chondrite-normalized platinum group elements (PGE) diagram. <sup>187</sup>Os/<sup>188</sup>Os isotopic ratios of the WOC are 0.12675 to 0.13011 and 0.11355 to 0.14421, coupled with <sup>187</sup>Re/<sup>188</sup>Os ratios of 0.0112 to 0.0272 and 0.0026 to 1.1869, for the chromitites and peridotites, respectively. These data suggest that the peridotites were modified by melt metasomatism and/or Re addition and chromitites formed by crystallization from melts. The Os isotopic composition of the chromitites reflects the isotopic composition of the melt. The calculated oxygen fugacities (ƒO<sub>2</sub>) values of the studied samples are moderate to high, with an oxidation state of log <i>f</i>O<sub>2</sub> units ranging from  − 0.17 to   +   0.99 for harzburgite,  +  0.37 to   +   1.63 for dunites and   +   0.52 to   +   2.84 for chromitites. The moderate to high oxidation state of the studied upper-mantle ophiolitic complexes suggests a boninitic source in the mantle wedge within an arc setting. In addition, the two-pyroxene thermometer presents mean equilibrium temperatures of 825°C, 841°C, 910°C and 910°C for harzburgite, lherzolite, dunite and pyroxenite samples, respectively. The spinel in lherzolites-harzburgites reflects the degree of depletion after tholeiitic melt extraction by proto-forearc spreading and infant arc generation, whereas spinel in dunites were affected by boninitic melt percolation and chromitites formed from boninitic melts during the mature proto-forearc stage, with a significant influence of slab-derived fluids at high ƒO<sub>2</sub>.
DOI: 10.6084/m9.figshare.28917410.v1
title: Petrological and Re-Os isotopic constraints on the origin of chromitites and peridotites of the late cretaceous Waziristan ophiolite, western Pakistan: implications for subduction initiation

description: The Waziristan Ophiolite Complex (WOC) occurs between the Afghan microplate in the west and the Indian plate in the east along the Main Waziristan Thrust in western Pakistan. A complete ophiolitic sequence, including residual lherzolites, harzburgites with foliated and discordant dunites, gabbroic rocks, dyke swarms, pillow and massive basaltic rocks, is present in the complex. Widespread podiform chromitites are usually enclosed by thin dunitic haloes in the complex. Chromian spinels in lherzolites-harzburgites are characterized by Cr# [= Cr/(Cr  +  Al)] values ranging from 0.19 to 0.60, and plot within or overlap the fields of abyssal to fore-arc peridotites, while chromian spinels in dunites and chromitites with Cr# values from 0.57 to 0.79 exhibit geochemical affinities similar to those of boninites. Trace element and REE characteristics, including the enrichment of light REE in the Waziristan Complex peridotites indicate the contribution of subduction-related fluids/melts, including boninitic mantle melts, validating a subduction initiation process in their genesis, and these features are similar to those observed in supra-subduction zone peridotites. Chromitites are characterized by enrichment of Os, Ir, Ru and Rh relative to Pt and Pd on a chondrite-normalized platinum group elements (PGE) diagram. <sup>187</sup>Os/<sup>188</sup>Os isotopic ratios of the WOC are 0.12675 to 0.13011 and 0.11355 to 0.14421, coupled with <sup>187</sup>Re/<sup>188</sup>Os ratios of 0.0112 to 0.0272 and 0.0026 to 1.1869, for the chromitites and peridotites, respectively. These data suggest that the peridotites were modified by melt metasomatism and/or Re addition and chromitites formed by crystallization from melts. The Os isotopic composition of the chromitites reflects the isotopic composition of the melt. The calculated oxygen fugacities (ƒO<sub>2</sub>) values of the studied samples are moderate to high, with an oxidation state of log <i>f</i>O<sub>2</sub> units ranging from  − 0.17 to   +   0.99 for harzburgite,  +  0.37 to   +   1.63 for dunites and   +   0.52 to   +   2.84 for chromitites. The moderate to high oxidation state of the studied upper-mantle ophiolitic complexes suggests a boninitic source in the mantle wedge within an arc setting. In addition, the two-pyroxene thermometer presents mean equilibrium temperatures of 825°C, 841°C, 910°C and 910°C for harzburgite, lherzolite, dunite and pyroxenite samples, respectively. The spinel in lherzolites-harzburgites reflects the degree of depletion after tholeiitic melt extraction by proto-forearc spreading and infant arc generation, whereas spinel in dunites were affected by boninitic melt percolation and chromitites formed from boninitic melts during the mature proto-forearc stage, with a significant influence of slab-derived fluids at high ƒO<sub>2</sub>.
DOI: 10.6084/m9.figshare.28943792
title: Small-scale manganese deposits in the Midwest of Brazil: geochemistry, Nd, Sr, and Pb isotopes, and a potential source of high-technology elements

description: In the Midwest of Brazil, several small manganese (Mn) deposits are located within the metavolcano-sedimentary rocks of the Paleoproterozoic Araí Group and the metasedimentary rocks of the Mesoproterozoic Paranoá Group. Mn occurs as layers, lamellae, fractures-filling, pocket-type, and blocks at the surface. For this study, 23 Mn ore samples from 12 small Mn-deposits were analysed using XRD, SEM, EPMA, and whole-rock geochemistry. This research aimed to identify the mineral and geochemical characteristics of these small Mn deposits, focusing on the geochemical associations, geological environment, source, and mineralization style of the Mn ores. This information facilitates the exploration of the influence of the Araí and Paranoá Groups as a potential source of Mn and critical and rare high-technology elements. Several stages of Mn mobilization were identified based on their geochemical differences, host geological units, and types of Mn occurrence. The Araí Group Mn deposit is characterized by hausmannite, cryptomelane, pyrolusite, and hollandite paragenesis, low P<sub>2</sub>O<sub>5</sub> contents, high Sr, Tl, and U concentrations, positive Eu/Eu* anomalies, high (La/Yb)<sub>N</sub>, and low Co/Zn ratios. These features suggest that the Mn deposit in the Araí Group had a metamorphic and hydrothermal overprint. The Paranoá Group Mn deposits are characterized by romanechite, lithiophorite, hollandite, cryptomelane, and pyrolusite paragenesis, high Al<sub>2</sub>O<sub>3</sub>, Ba, Co, Cu, and Ni concentrations, high Co/Zn ratios, and LREE UCC depletion. These features indicate an interplay of older sources, tectonic deformation, and surficial weathering. Moreover, the high content of Ba, Co, Cu, Ni, Sr, Tl, U, Y, and REE in the Mn deposits makes them suppliers of critical and rare high-technology elements.
DOI: 10.6084/m9.figshare.28943792.v1
title: Small-scale manganese deposits in the Midwest of Brazil: geochemistry, Nd, Sr, and Pb isotopes, and a potential source of high-technology elements

description: In the Midwest of Brazil, several small manganese (Mn) deposits are located within the metavolcano-sedimentary rocks of the Paleoproterozoic Araí Group and the metasedimentary rocks of the Mesoproterozoic Paranoá Group. Mn occurs as layers, lamellae, fractures-filling, pocket-type, and blocks at the surface. For this study, 23 Mn ore samples from 12 small Mn-deposits were analysed using XRD, SEM, EPMA, and whole-rock geochemistry. This research aimed to identify the mineral and geochemical characteristics of these small Mn deposits, focusing on the geochemical associations, geological environment, source, and mineralization style of the Mn ores. This information facilitates the exploration of the influence of the Araí and Paranoá Groups as a potential source of Mn and critical and rare high-technology elements. Several stages of Mn mobilization were identified based on their geochemical differences, host geological units, and types of Mn occurrence. The Araí Group Mn deposit is characterized by hausmannite, cryptomelane, pyrolusite, and hollandite paragenesis, low P<sub>2</sub>O<sub>5</sub> contents, high Sr, Tl, and U concentrations, positive Eu/Eu* anomalies, high (La/Yb)<sub>N</sub>, and low Co/Zn ratios. These features suggest that the Mn deposit in the Araí Group had a metamorphic and hydrothermal overprint. The Paranoá Group Mn deposits are characterized by romanechite, lithiophorite, hollandite, cryptomelane, and pyrolusite paragenesis, high Al<sub>2</sub>O<sub>3</sub>, Ba, Co, Cu, and Ni concentrations, high Co/Zn ratios, and LREE UCC depletion. These features indicate an interplay of older sources, tectonic deformation, and surficial weathering. Moreover, the high content of Ba, Co, Cu, Ni, Sr, Tl, U, Y, and REE in the Mn deposits makes them suppliers of critical and rare high-technology elements.
DOI: 10.6084/m9.figshare.28978346
title: Delta sedimentary evolution: a comprehensive review and perspectives on construction and destruction

description: The study of constructive–destructive deltas is crucial for exploring and developing oil and gas reservoirs in rocky formations. Current scholarly research has allocated limited attention to the factors governing both the constructive and destructive aspects. This review, from a constructive–destructive perspective, examines various factors influencing the evolution of constructive–destructive deltas since their formation. It dissects the sedimentary evolution of these deltas, quantitatively analyzes the identification factors of the destruction conversion surface of delta construction, explains the significance of research on destructive delta construction for the exploration and development of rocky stratigraphic reservoirs, and summarizes the multidisciplinary background and development dynamics. These approaches deepen our understanding of the process–product relationship, delta formation and evolution dynamics, and resource dynamics. This review advances the vitality of delta studies, advances further research on delta classification, and improves the accuracy of interpreting the deltaic sediment transport and depositional mechanisms. Additionally, it allows for the quantification of depositional group structure, distribution of zones, and stratigraphic sequence of delta sedimentary structures.
DOI: 10.6084/m9.figshare.28978346.v1
title: Delta sedimentary evolution: a comprehensive review and perspectives on construction and destruction

description: The study of constructive–destructive deltas is crucial for exploring and developing oil and gas reservoirs in rocky formations. Current scholarly research has allocated limited attention to the factors governing both the constructive and destructive aspects. This review, from a constructive–destructive perspective, examines various factors influencing the evolution of constructive–destructive deltas since their formation. It dissects the sedimentary evolution of these deltas, quantitatively analyzes the identification factors of the destruction conversion surface of delta construction, explains the significance of research on destructive delta construction for the exploration and development of rocky stratigraphic reservoirs, and summarizes the multidisciplinary background and development dynamics. These approaches deepen our understanding of the process–product relationship, delta formation and evolution dynamics, and resource dynamics. This review advances the vitality of delta studies, advances further research on delta classification, and improves the accuracy of interpreting the deltaic sediment transport and depositional mechanisms. Additionally, it allows for the quantification of depositional group structure, distribution of zones, and stratigraphic sequence of delta sedimentary structures.
DOI: 10.5281/zenodo.8346838
title: Testing Context-Aware Software Systems in the Automotive Domain: A Multi Vocal Literature Review Protocol and Dataset

description: Testing Context-Aware Software Systems in the Automotive Domain: A Multi Vocal Literature Review Protocol and Dataset
A Multi-Vocal Literature Review (MVLR) is a form of a systematic review that includes grey literature in addition to peer-review literature (Garousi, Felderer, and Mäntylä 2019). The decision to justify an MVLR is drawn from the results of recent literature reviews, in particular the recent results from (Matalonga et al. 2022)  where it is shown that there is little evidence in the white literature on the approaches to testing non-academic CASS Systems.
Previous academic works (including our Quasi-Systematic Literature Reviews and Rapid Reviews) operate under the following assumptions and observations:

Assumption 1. CASS are widespread and being deployed for commercial or industrial use.
Observation 1. The software engineering and software testing communities have had time to adopt (or develop new) techniques to deal with the context and effects of testing software systems.
Observation 2. Academics have been able to work with software organizations to transfer or study the approaches used to test CASS, yet the published case studies we are aware of describe a partial picture of the overall adoption and approach of the problem.
In spite of these assumptions and the availability of systematic literature review studies, there is little evidence of how software organizations are testing CASS.
Research Goals
Aim: To uncover evidence on how the automotive industry reports their working with the dynamic testing process regarding CASS.
We use the term industry to broaden our scope to include stakeholders with an interest in the quality of CASS like NGOs, standard-setting organizations and regulation-setting organizations who can influence how software must be treated in different domains.
The following research questions convey the general interest of our enquiries. These are driven by our previous research and expectations on the sources.

RQ1 Are there sources to support the understanding and indicate directions to deal with the problem of testing CASS?
RQ2 What are the challenges of using these dynamic testing process solutions?
RQ3 How are the dynamic testing processes that deal with the context of CASS described in the sources?
Dataset 
This dataset contains the following artifacts:

Testing CASS MVLR Protocol.pdf: protocol containing the methodological details of performing the MVLR
Sources Identification, Selection and Data Extraction.xlsx: spreadsheet used to record and control discovered and selected sources
Extraction_Documents.zip: compressed file containing all data collection forms filled with data extracted from the
MVLR_Analysis-Codebook.xlsx: listing of codes emerging from the collected data
DOI: 10.5281/zenodo.8346839
title: Testing Context-Aware Software Systems in the Automotive Domain: A Multi Vocal Literature Review Protocol and Dataset

description: Testing Context-Aware Software Systems in the Automotive Domain: A Multi Vocal Literature Review Protocol and Dataset
A Multi-Vocal Literature Review (MVLR) is a form of a systematic review that includes grey literature in addition to peer-review literature (Garousi, Felderer, and Mäntylä 2019). The decision to justify an MVLR is drawn from the results of recent literature reviews, in particular the recent results from (Matalonga et al. 2022)  where it is shown that there is little evidence in the white literature on the approaches to testing non-academic CASS Systems.
Previous academic works (including our Quasi-Systematic Literature Reviews and Rapid Reviews) operate under the following assumptions and observations:

Assumption 1. CASS are widespread and being deployed for commercial or industrial use.
Observation 1. The software engineering and software testing communities have had time to adopt (or develop new) techniques to deal with the context and effects of testing software systems.
Observation 2. Academics have been able to work with software organizations to transfer or study the approaches used to test CASS, yet the published case studies we are aware of describe a partial picture of the overall adoption and approach of the problem.
In spite of these assumptions and the availability of systematic literature review studies, there is little evidence of how software organizations are testing CASS.
Research Goals
Aim: To uncover evidence on how the automotive industry reports their working with the dynamic testing process regarding CASS.
We use the term industry to broaden our scope to include stakeholders with an interest in the quality of CASS like NGOs, standard-setting organizations and regulation-setting organizations who can influence how software must be treated in different domains.
The following research questions convey the general interest of our enquiries. These are driven by our previous research and expectations on the sources.

RQ1 Are there sources to support the understanding and indicate directions to deal with the problem of testing CASS?
RQ2 What are the challenges of using these dynamic testing process solutions?
RQ3 How are the dynamic testing processes that deal with the context of CASS described in the sources?
Dataset 
This dataset contains the following artifacts:

Testing CASS MVLR Protocol.pdf: protocol containing the methodological details of performing the MVLR
Sources Identification, Selection and Data Extraction.xlsx: spreadsheet used to record and control discovered and selected sources
Extraction_Documents.zip: compressed file containing all data collection forms filled with data extracted from the
MVLR_Analysis-Codebook.xlsx: listing of codes emerging from the collected data
DOI: 10.6084/m9.figshare.28903644
title: Whole rock geochemistry, zircon U-Pb dating and Sr-Nd and Hf isotopic studies of Cretaceous granitoids from Southern Pamir, Tajikistan: insights into Pamir Plateau formation

description: The Southern Pamir region, a critical part of the Alpine-Himalayan orogenic belt, exhibits a complex tectonomagmatic history that offers insights into the geodynamic evolution of the Pamir Plateau. This study presents comprehensive data on the Cretaceous granitoids from the Kyzylrabat area, including whole-rock geochemistry, zircon U-Pb geochronology and Sr-Nd-Hf isotopic analyses. The analysed granitoids are high-K calc-alkaline to shoshonitic, exhibiting A-type geochemical signatures. Zircon U-Pb ages range from 98.5 to 111.7 Ma, correlating well with contemporaneous volcanic activities. Isotopic data indicate a mixed magmatic origin involving a mantle-derived high-K magma and a crustal-derived felsic component. Petrogenetic analyses reveal co-magmatic trends and magma mixing processes, with geochemical evidence suggesting a mantle source metasomatized by subduction-related fluids. Geodynamic interpretations propose that the granitoids formed in an extensional back-arc setting during the northward subduction of the Shyok branch of the Neotethys Ocean. These findings provide critical constraints on the mid-Cretaceous tectonic and magmatic processes in the Southern Pamir, contributing to a deeper understanding of the orogenic plateau formation and evolution.
DOI: 10.6084/m9.figshare.28903644.v1
title: Whole rock geochemistry, zircon U-Pb dating and Sr-Nd and Hf isotopic studies of Cretaceous granitoids from Southern Pamir, Tajikistan: insights into Pamir Plateau formation

description: The Southern Pamir region, a critical part of the Alpine-Himalayan orogenic belt, exhibits a complex tectonomagmatic history that offers insights into the geodynamic evolution of the Pamir Plateau. This study presents comprehensive data on the Cretaceous granitoids from the Kyzylrabat area, including whole-rock geochemistry, zircon U-Pb geochronology and Sr-Nd-Hf isotopic analyses. The analysed granitoids are high-K calc-alkaline to shoshonitic, exhibiting A-type geochemical signatures. Zircon U-Pb ages range from 98.5 to 111.7 Ma, correlating well with contemporaneous volcanic activities. Isotopic data indicate a mixed magmatic origin involving a mantle-derived high-K magma and a crustal-derived felsic component. Petrogenetic analyses reveal co-magmatic trends and magma mixing processes, with geochemical evidence suggesting a mantle source metasomatized by subduction-related fluids. Geodynamic interpretations propose that the granitoids formed in an extensional back-arc setting during the northward subduction of the Shyok branch of the Neotethys Ocean. These findings provide critical constraints on the mid-Cretaceous tectonic and magmatic processes in the Southern Pamir, contributing to a deeper understanding of the orogenic plateau formation and evolution.
DOI: 10.15468/dl.zrkxxu
title: Occurrence Download

description: A dataset containing 161440 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasCoordinate is true",
 "TaxonKey is Ononis spinosa procurrens"
 ]
}

 The dataset includes 161440 records from 942 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0015722-250827131500795/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.29673487
title: Dox-HCl and miR-145 co-delivery through CD44-targeted PEGylated liposomes inhibit Breast Cancer <i>in vitro</i> via augmenting PI3K/AKT pathway

description: The aim of this study deals with integrating a CD44-targeting short peptide, A6 (KPSSPPEE) onto the PEGylated liposomes to enhance the in vitro anticancer activities of doxorubicin hydrochloride and tumor suppressor miR-145 mimics on triple-negative breast cancer. A CD44-targeting short peptide, A6 (KPSSPPEE) was integrated onto the optimized PEGylated liposomes, and its effects on cellular uptake, anti-proliferation, and anti-metastasis activities were assessed in triple-negative breast cancer, MDA-MB-231 cells. The resulting formulation (A6-PEG-lipo-Dox-miR145) demonstrated enhanced cellular uptake by CD44-expressing MDA-MB-231 cells within 2 h of incubation. In vitro study showed that A6-PEG-lipo-Dox-miR145 exerted a greater anti-proliferative activity with higher selectivity (Dox-HCl IC<sub>50</sub> = 1.60 ± 0.07 μM; selectivity index (SI) = 1.30) against MDA-MB-231 cells when compared to MCF10A cells, which an enhanced suppression of PI3K/AKT pathway was observed, highlighting its potential as a targeted therapy for TNBC. Additionally, A6-PEG-lipo-Dox-miR145 showed anti-migration and improved anti-invasion activities on MDA-MB-231 cells, which correlated with its ability in reversing endothelial-to-mesenchymal transition (EMT) through modulating both N-cadherin and E-cadherin expression. Our findings indicate that the incorporation of A6 peptide represents a simple and straightforward strategy to improve the targetability and therapeutic effects of PEGylated liposome, warranting further investigation.