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Remote Detection of Hydrocarbon Microseepage in a Loess Covered Area

Remote Detection of Hydrocarbon Microseepage in a Loess Covered Area

作     者:Liang Zhao Darning Wang Shengbo Chen Lin Li Tianyu Zhang Liang Zhao;Daming Wang;Shengbo Chen;Lin Li;Tianyu Zhang

作者机构:College of Geo-Exploration Science and TechnologyJilin UniversityChangchun 130026China Division of Petroleum GeologyChina Geological SurveyBeijing 100037China Department of Earth SciencesIndiana University-Purdue University IndianapolisIndianapolis 46202USA College of Earth ScienceJilin UniversityChangchun 130061China 

出 版 物:《Journal of Earth Science》 (地球科学学刊(英文版))

年 卷 期:2020年第31卷第1期

页      面:207-214页

核心收录:

学科分类:081801[工学-矿产普查与勘探] 081803[工学-地质工程] 08[工学] 0708[理学-地球物理学] 0818[工学-地质资源与地质工程] 0704[理学-天文学] 

基  金:supported by the National Natural Science Foundation of China(No.41402293) the GF-5 Satellite Hyperspectral Porphyry Deposit Alteration Information Intelligent Identification Technology Program(No.04-Y20A35-9001-15/17-4) 

主  题:hyperspectral remote sensing hydrocarbon microseepage spectrum absorption parameters multiple regression analysis fast index geochemistry 

摘      要:Hydrocarbon microseepage can result in related near-surface mineral *** this study,we evaluated the potential of detecting these alterations with field measured and satellite acquired hyperspectral *** soil samples and reflectance spectra were collected in the Xifeng Oilfield,a loess covered *** samples were analyzed in the laboratory for calcite,dolomite,kaolinite,illite,and mixedlayer illite/smectite content,and we processed reflectance spectra for continuum removal to derive clay and carbonate mineral absorption depth(H).High correlation between absorption depth and mineral content was shown for clay and mineral carbonate with field measured *** on the result for the field spectra,we proposed and tested a fast index based on the absorption depth of clay and carbonate minerals with a hyperspectral image of the *** detected hydrocarbon microseepage anomalies matched well with those shown in the geological map.

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