China Geology最新文献

{"title":"Health risk assessment of heavy metals in soils and crops in a mining area (Au-Ag-Cu-trona-oil et al.) of the Nanyang Basin, Henan Province, China","authors":"Qiu-yao Dong ,&nbsp;Hao-tian Wen ,&nbsp;Pan Wang ,&nbsp;Chao Song ,&nbsp;Shu-ya Lai ,&nbsp;Zhen-jing Yang ,&nbsp;Yuan-yi Zhao ,&nbsp;Ming-jiang Yan","doi":"10.31035/cg2022078","DOIUrl":"10.31035/cg2022078","url":null,"abstract":"<div><p>Heavy metal distribution in mining areas has always been a hot research topic due to the special environment of these areas. This study aims to explore the impact of heavy metal pollution on soils and crops in the study area, ensure the safety of local crops and the health of local residents, and provide a basis for the subsequent environmental restoration and the prevention and control of environmental pollution. Based on the analysis of the heavy metal concentrations in local soils and crops, the study investigated the spatial distribution, pollution degrees, and potential ecological risks of heavy metals in the farmland of a mining area in the southeastern Nanyang Basin, Henan province, China explored the sources of heavy metals and assessed the health risks caused by crop intake. The results of this study are as follows. The root soils of crops in the study area suffered heavy metal pollution to varying degrees. The degree of heavy metal pollution in maize fields is higher than that in wheat fields, and both types of fields suffer the most severe Cd pollution. Moreover, the root soils of different crops suffer compound pollution. The root soils in the maize fields suffer severe compound pollution at some sampling positions, whose distribution is similar to that of the mining area. Cd poses the highest potential ecological risks among all heavy metals, and the study area mainly suffers low and moderate comprehensive potential ecological risks. The principal component analysis (PCA) shows that the distribution of Zn, Cd, Pb, and As in soils of the study area is mainly affected by anthropogenic factors such as local mining activities; the distribution of Cr and Ni is primarily controlled by the local geological background; the distribution of Hg is mainly affected by local vehicle exhaust emissions, and the distribution of Cu is influenced by both human activities and the geological background. Different cereal crops in the study area are polluted with heavy metals dominated by Cd and Ni to varying degrees, especially wheat. As indicated by the health risk assessment results, the intake of maize in the study area does not pose significant human health risks; however, Cu has high risks to human health, and the compound heavy metal pollution caused by the intake of wheat in the study area poses risks to the health of both adults and children. Overall, the soils and crops in the study area suffer a high degree of heavy metal pollution, for which mining activities may be the main reason.</p><p>©2023 China Geology Editorial Office.</p></div>","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"6 4","pages":"Pages 567-579"},"PeriodicalIF":4.5,"publicationDate":"2023-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2096519223014921/pdfft?md5=6ccc49ef92b94ad15b17df2d84b85344&pid=1-s2.0-S2096519223014921-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"78248523","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"A three-dimensional Moho depth model beneath the Yemeni highlands and rifted volcanic margins of the Red Sea and Gulf of Aden, Southwest Arabia","authors":"Amin Noman Al Kadasi","doi":"10.31035/cg2023001","DOIUrl":"10.31035/cg2023001","url":null,"abstract":"<div><p>Knowing Moho discontinuity undulation is fundamental to understanding mechanisms of lithosphere-asthenosphere interaction, extensional tectonism and crustal deformation in volcanic passive margins such as the study area, which is located in the southwestern corner of the Arabian Peninsula bounded by the Red Sea and the Gulf of Aden. In this work, a 3D Moho depth model of the study area is constructed for the first time by inverting gravity data from the Earth Gravitational Model (EGM2008) using the Parker-Oldenburg algorithm. This model indicates the shallow zone is situated at depths of 20 km to 24 km beneath coastal plains, whereas the deep zone is located below the plateau at depths of 30 km to 35 km and its deepest part coincides mainly with the Dhamar-Rada’a Quaternary volcanic field. The results also indicate two channels of hot magmatic materials joining both the Sana’a-Amran Quaternary volcanic field and the Late Miocene Jabal An Nar volcanic area with the Dhamar-Rada’a volcanic field. This conclusion is supported by the widespread geothermal activity (of mantle origin) distributed along these channels, isotopic data, and the upper mantle low velocity zones indicated by earlier studies.</p><p>©2023 China Geology Editorial Office.</p></div>","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"6 4","pages":"Pages 611-622"},"PeriodicalIF":4.5,"publicationDate":"2023-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2096519223014957/pdfft?md5=d2b086748cfbd765d0b83db18ceb58ec&pid=1-s2.0-S2096519223014957-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"87231309","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Zircon U-Pb age of the volcanic rock from the Huoshiling Formation in the Yingtai Fault Depression, Songliao Basin, China","authors":"Cheng-long Wang ,&nbsp;Li-bin Song ,&nbsp;Hong-qi Yuan","doi":"10.31035/cg2023002","DOIUrl":"10.31035/cg2023002","url":null,"abstract":"","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"6 4","pages":"Pages 751-752"},"PeriodicalIF":4.5,"publicationDate":"2023-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2096519223015033/pdfft?md5=a3d6a0c43130bf2778a62c042f0c4895&pid=1-s2.0-S2096519223015033-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"76884074","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Identification of clayey altered ophiolite in the Nujiang tectonic belt and new understanding of its impacts on engineering stability","authors":"Jin-qiu Li ,&nbsp;Yong-shuang Zhang ,&nbsp;Xue Li ,&nbsp;San-shao Ren ,&nbsp;Li-na Ran","doi":"10.31035/cg2023076","DOIUrl":"https://doi.org/10.31035/cg2023076","url":null,"abstract":"","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"6 4","pages":"Pages 756-758"},"PeriodicalIF":4.5,"publicationDate":"2023-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2096519223015057/pdfft?md5=5c1ecdb80583f5d6d1e845b005e73bd8&pid=1-s2.0-S2096519223015057-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"138738771","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Geology and mineralization of the Bayan Obo supergiant carbonatite-type REE-Nb-Fe deposit in Inner Mongolia, China: A review","authors":"Yi-ke Li ,&nbsp;Chang-hui Ke ,&nbsp;Hong-quan She ,&nbsp;Deng-hong Wang ,&nbsp;Cheng Xu ,&nbsp;An-jian Wang ,&nbsp;Rui-ping Li ,&nbsp;Zi-dong Peng ,&nbsp;Ze-ying Zhu ,&nbsp;Kui-feng Yang ,&nbsp;Wei Chen ,&nbsp;Jian-wei Zi ,&nbsp;Wen-lei Song ,&nbsp;Yong-gang Zhao ,&nbsp;Li Zhang ,&nbsp;Hong Yu ,&nbsp;Bin Guo ,&nbsp;Sheng-quan Zhou ,&nbsp;Xing-yu Yuan ,&nbsp;Jing-yao Liu","doi":"10.31035/cg2023082","DOIUrl":"https://doi.org/10.31035/cg2023082","url":null,"abstract":"<div><p>The Bayan Obo supergiant carbonatite-related rare-earth-element-niobium-iron (REE-Nb-Fe) endogenetic deposit (thereafter as the Bayan Obo deposit), located at 150 km north of Baotou City in the Inner Mongolia Autonomous Region, is the largest rare-earth element (REE) resource in the world. Tectonically, this deposit is situated on the northern margin of the North China Craton and adjacent to the Xing’an-Mongolian orogenic belt to the south. The main strata within the mining area include the Neoarchean Se’ ertengshan Group and the Mesoproterozoic Bayan Obo Group. Generally, the rare earth, niobium, and iron mineralization within the deposit are intrinsically related to the dolomite carbonatites and the extensive alteration of the country rocks caused by the carbonatite magma intrusion. The alteration of country rocks can be categorized into three types: contact metasomatism (anti-skarn and skarn alteration), fenitization, and hornfelsic alternation. As indicated by previous studies and summarized in this review, the multi-element mineralization at Bayan Obo is closely associated with the metasomatic replacement of siliceous country rocks by carbonatite magmatic-hydrothermal fluids. The metasomatic process is comparable to the conventional skarnification that formed due to the intrusion of intermediate-acid magmatic rocks into limestone strata. However, the migration pattern of SiO₂, CaO, and MgO in this novel metasomatic process is opposite to the skarn alteration. Accordingly, this review delineates, for the first time, an anti-skarn metallogenic model for the Bayan Obo deposit, revealing the enigmatic relationship between the carbonatite magmatic-hydrothermal processes and the related iron and rare earth mineralization. Moreover, this study also contributes to a better understanding of the REE-Nd-Fe metallogenetic processes and the related fluorite mineralization at the Bayan Obo deposit.</p><p>©2023 China Geology Editorial Office.</p></div>","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"6 4","pages":"Pages 716-750"},"PeriodicalIF":4.5,"publicationDate":"2023-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2096519223015021/pdfft?md5=f1803cea166fd4c76fae82601510cb41&pid=1-s2.0-S2096519223015021-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"138739105","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Biophysical warming patterns of an open-top chamber and its short-term influence on a Phragmites wetland ecosystem in China","authors":"Xue-yang Yu ,&nbsp;Si-yuan Ye ,&nbsp;Li-xin Pei ,&nbsp;Liu-juan Xie ,&nbsp;Ken W. Krauss ,&nbsp;Samantha K. Chapman ,&nbsp;Hans Brix","doi":"10.31035/cg2022064","DOIUrl":"10.31035/cg2022064","url":null,"abstract":"<div><p>Passive-warming, open-top chambers (OTCs) are widely applied for studying the effects of future climate warming on coastal wetlands. In this study, a set of six OTCs were established at a <em>Phragmites</em> wetland located in the Yellow River Delta of Dongying City, China. With data collected through online transmission and <em>in-situ</em> sensors, the attributes and patterns of realized OTCs warming are demonstrated. The authors also quantified the preliminary influence of experimental chamber warming on plant traits. OTCs produced an elevated average air temperature of 0.8°C (relative to controls) during the growing season (June to October) of 2018, and soil temperatures actually decreased by 0.54°C at a depth of 5 cm and 0.46°C at a depth of 30 cm in the OTCs. Variations in diel patterns of warming depend greatly on the heat sources of incoming radiation in the daytime versus soil heat flux at night. Warming effects were often larger during instantaneous analyses and influenced OTCs air temperatures from −2.5°C to 8.3°C dependent on various meteorological conditions at any given time, ranging from cooling influences from vertical heat exchange and vegetation to radiation-associated warming. Night-time temperature depressions in the OTCs were due to the low turbulence inside OTCs and changes in surface soil-atmosphere heat transfer. Plant shoot density, basal diameter, and biomass of <em>Phragmites</em> decreased by 23.2%, 6.3%, and 34.0%, respectively, under experimental warming versus controls, and plant height increased by 4.3%, reflecting less carbon allocation to stem structures as plants in the OTCs experienced simultaneous wind buffering. While these passive-warming OTCs created the desired warming effects both to the atmosphere and soils, pest damages on the plant leaves and lodging within the OTCs were extensive and serious, creating the need to consider control options for these chambers and the replicated OTCs studies underway in other Chinese <em>Phragmites</em> marshes (Panjin and Yancheng).</p><p>©2023 China Geology Editorial Office.</p></div>","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"6 4","pages":"Pages 594-610"},"PeriodicalIF":4.5,"publicationDate":"2023-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2096519223014945/pdfft?md5=f4aa24926986a29f3bd7c69b3993217c&pid=1-s2.0-S2096519223014945-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"80108911","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Application of the monitoring and early warning system for internal solitary waves: Take the second natural gas hydrates production test in the South China Sea as an example","authors":"Dan-yi Su ,&nbsp;Bin-bin Guo ,&nbsp;Qian-yong Liang ,&nbsp;Chu-jin Liang ,&nbsp;Fei-long Lin ,&nbsp;Su-meng Jiang ,&nbsp;Yi-fei Dong ,&nbsp;Xue-min Wu","doi":"10.31035/cg2022043","DOIUrl":"https://doi.org/10.31035/cg2022043","url":null,"abstract":"<div><p>Internal solitary waves (ISWs) contain great energy and have the characteristics of emergency and concealment. To avoid their damage to offshore engineering, a new generation of monitoring and early warning system for ISWs was developed using technologies of double buoys monitoring, intelligent real-time data transmission, and automatic software identification. The system was applied to the second natural gas hydrates (NGHs) production test in the Shenhu Area, South China Sea (SCS) and successfully provided the early warning of ISWs for 173 days (from October 2019 to April 2020). The abrupt changes in the thrust force of the drilling platform under the attack of ISWs were consistent with the early warning information, proving the reliability of this system. A total of 93 ISWs were detected around the drilling platform. Most of them occurred during the spring tides in October–December 2019 and April 2020, while few of them occurred in winter. As suggested by the theoretical model, the full-depth structure of ISWs was a typical current profile of mode-1, and the velocities of wave-induced currents can reach 80 cm/s and 30 cm/s, respectively, in the upper ocean and near the seabed. The ISWs may be primarily generated from the interactions between the topography and semidiurnal tides in the Luzon Strait, and then propagate westward to the drilling platform. This study could serve as an important reference for the early warning of ISWs for offshore engineering construction in the future.</p><p>©2023 China Geology Editorial Office.</p></div>","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"6 4","pages":"Pages 676-684"},"PeriodicalIF":4.5,"publicationDate":"2023-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2096519223014994/pdfft?md5=4fc0797c2f99557d70c8e9f34b1f9910&pid=1-s2.0-S2096519223014994-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"138739112","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Tectonic evolution and accumulation characteristics of Carboniferous shale gas in Yadu-Ziyun-Luodian aulacogen, Guizhou Province, South China","authors":"Kun Yuan ,&nbsp;Wen-hui Huang ,&nbsp;Ting Wang ,&nbsp;Shi-zhen Li ,&nbsp;Xiang-can Sun ,&nbsp;Xin-xin Fang ,&nbsp;Jun-ping Xiao ,&nbsp;Jun Guo","doi":"10.31035/cg2022059","DOIUrl":"10.31035/cg2022059","url":null,"abstract":"<div><p>The Yadu-Ziyun-Luodian aulacogen (YZLA) developed into being NW-trending in the Late Paleozoic, and was considered as an important passive continental margin aulacogen in Guizhou Province, South China. This tectonic zone is considered a large intracontinental thrust-slip tectonic unit, which has undergone a long period of development. It was ultimately determined in the Yanshanian, where the typical Upper Paleozoic marine shales were deposited. In 2021, Well QSD-1 was deployed in the Liupanshui area at the northwest margin of the aulacogen, and obtained a daily shale gas flow of 11011 m³ in the Carboniferous Dawuba Formation. It thus achieved a breakthrough in the invesgation of shale gas in the Lower Carboniferous in South China, revealing relatively good gas-bearing properties and broad exploration prospects of the aulacogen. Being different from the Lower Paleozoic strata in the Sichuan Basin and the Yichang area of the Middle Yangtze, the development of the Carboniferous Dawuba Formation in the aulacogen exhibits the following characteristics: (1) The Lower Carboniferous shale is thick and widely distributed, with interbedded shale and marlstone of virous thickness; (2) The total organic carbon (TOC) content of the shale in the Dawuba Formation ranges from 1% to 5%, with an average of 2%, and the thermal maturity of organic matter (<em>R</em>_o) varies from 1% to 4%, with an average of 2.5%, indicating good hydrocarbon generation capacity; (3) The main shale in the aulacogen was formed during the fault subsidence stage from the Middle Devonian to the Early Permian. Although the strong compression and deformation during the late Indosinian-Himalayan played a certain role in destroying the formed shale gas reservoirs, comparative analysis suggests that the area covered by the current Triassic strata has a low degree of destruction. It therefore provides good conditions for shale gas preservation, which can be regarded as a favorable area for the next exploration.</p><p>©2023 China Geology Editorial Office.</p></div>","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"6 4","pages":"Pages 646-659"},"PeriodicalIF":4.5,"publicationDate":"2023-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2096519223014970/pdfft?md5=32ab75612d49257dcaabd824f89a5cf5&pid=1-s2.0-S2096519223014970-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"79549331","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"The accumulation characteristics and exploration potential of oil and gas in the back-arc basin of Japan under the background of high heat flow","authors":"Jian-qiang Wang ,&nbsp;Jie Liang ,&nbsp;Jian-wen Chen ,&nbsp;Qing-fang Zhao ,&nbsp;Yin-guo Zhang ,&nbsp;Jian-wei Zhang ,&nbsp;Sen Li ,&nbsp;Chang-qing Yang ,&nbsp;Jian Zhang ,&nbsp;Jing Sun ,&nbsp;Chuan-sheng Yang ,&nbsp;Yong Yuan ,&nbsp;Lee-Jel Jiang","doi":"10.31035/cg2022067","DOIUrl":"10.31035/cg2022067","url":null,"abstract":"<div><p>The Sea of Japan is located in the southeast margin of Eurasia, in the triangle area of the western Pacific Ocean. Due to the interaction of the Pacific plate, Eurasian plate and Philippine plate, its tectonic environment is complex, forming a typical trench-arc-basin system. At present, 148 oil and gas fields have been discovered in Japan, with an oil and gas resource of 255.78×10⁶ t, showing a good prospect for oil and gas exploration. Based on the previous research and the recently collected geological and geophysical data, the characteristics of tectonic-sedimentary evolution and geothermal field in the basins around the Sea of Japan are analyzed. The results show that the tectonic evolution of the basin is mainly controlled by plate subduction and back-arc oceanic crust expansion, and it mainly undergone four tectonic-sedimentary evolution stages: Subduction period, basin development period, subsidence period and compression deformation period. The overall heat flow value of Japan Sea is high, and it is distributed annularly along Yamato Ridge. The geothermal heat flow value is about 50–130 MW/m², and the average heat flow is 75.9±19.8 MW/m², which has a typical “hot basin”. The high heat flow background provides unique thermal evolution conditions for hydrocarbon generation, which leads to the high temperature and rapid evolution. The authors summarized as “early hydrocarbon generation, rapid maturity and shallow and narrow hydrocarbon generation window”. The type of oil and gas is mainly natural gas, and it mainly distributed in Neogene oil and gas reservoirs. The trap types are mainly structural traps, lithologic traps and composite traps. In addition, the pre-Neogene bedrock oil and gas reservoirs also show a good exploration prospect. The resource prospecting indicates that Niigata Basin, Ulleung Basin and kitakami Basin are the main target areas for future exploration and development.</p><p>©2023 China Geology Editorial Office.</p></div>","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"6 4","pages":"Pages 660-675"},"PeriodicalIF":4.5,"publicationDate":"2023-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2096519223014982/pdfft?md5=21b5827c0597b5795a20a84a3f560a40&pid=1-s2.0-S2096519223014982-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"79644534","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Reply: Comment on “Geological mapping and mining prospecting in the Aouli inlier (Eastern Meseta, Morocco) based on remote sensing and geographic information systems (GIS)” by Benaissi et al. (China Geology, 5 (2022))","authors":"Lakhlifa Benaissi ,&nbsp;Adnane Tobi ,&nbsp;Khalid El Amari ,&nbsp;Mohamed Hibti","doi":"10.31035/cg2023074","DOIUrl":"https://doi.org/10.31035/cg2023074","url":null,"abstract":"","PeriodicalId":45329,"journal":{"name":"China Geology","volume":"6 4","pages":"Pages 762-766"},"PeriodicalIF":4.5,"publicationDate":"2023-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2096519223015070/pdfft?md5=598d049b7e1746cc48a9d44cbc48e71a&pid=1-s2.0-S2096519223015070-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"138738802","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}