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FORMATION CONDITIONS OF JIMUSAER OIL SHALE AT THE NORTHERN FOOT OF BOGDA MOUNTAIN, CHINA
The Jimusaer oil shale, located in the northern foot of Bogda Mountain, was deposited in the Lucaogou Formation in the Upper Permian. In this paper the effect of paleostructure, paleoclimate and sedimentary environment on the mineralization of oil shale in the study area was investigated. The result...
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Published in: | Oil shale (Tallinn, Estonia : 1984) Estonia : 1984), 2014-01, Vol.31 (1), p.19-19 |
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creator | Liang, Jianlong Tang, Dazhen Xu, Hao Tao, Shu Li, Chenchen Gou, Mingfu |
description | The Jimusaer oil shale, located in the northern foot of Bogda Mountain, was deposited in the Lucaogou Formation in the Upper Permian. In this paper the effect of paleostructure, paleoclimate and sedimentary environment on the mineralization of oil shale in the study area was investigated. The results show that, the Jimusaer oil shale was developed in the stable paralic lacustrine basin formed in the Late Middle Permian, and cropped out with the uplift of Bogda Mountain during the Himalayan orogeny. The Lucaogou Formation, which is composed of six lithologic segments, was deposited in a warm humid to dry hot climate and fresh to brackish water environment indicated by values of Sr/Cu, Sr/Ba and Mn/Fe ratios, which vary segment by segment. There are also similar variety regularities shown, which implicate that, the changes of paleoclimate influenced directly water salinity in the study area. |
doi_str_mv | 10.3176/oil.2014.1.03 |
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CONDITIONS OF JIMUSAER OIL SHALE AT THE NORTHERN FOOT OF BOGDA MOUNTAIN, CHINA</title><author>Liang, Jianlong ; Tang, Dazhen ; Xu, Hao ; Tao, Shu ; Li, Chenchen ; Gou, Mingfu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a500t-80c722be4b22427ccbd458b8f5ab1ed4dfaf759de90333de98dc0e9a6c46055b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Basins</topic><topic>Brackish</topic><topic>Brackish water</topic><topic>Climate</topic><topic>Deposition</topic><topic>Drying</topic><topic>Freshwater</topic><topic>Geological research</topic><topic>Lithology</topic><topic>Mineralization</topic><topic>Mountains</topic><topic>Oil shale</topic><topic>Oil-shales</topic><topic>Paleoclimatology</topic><topic>Properties</topic><topic>Saline water</topic><topic>Salinity</topic><topic>Sedimentation</topic><topic>Segments</topic><topic>Strontium</topic><topic>Trace 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In this paper the effect of paleostructure, paleoclimate and sedimentary environment on the mineralization of oil shale in the study area was investigated. The results show that, the Jimusaer oil shale was developed in the stable paralic lacustrine basin formed in the Late Middle Permian, and cropped out with the uplift of Bogda Mountain during the Himalayan orogeny. The Lucaogou Formation, which is composed of six lithologic segments, was deposited in a warm humid to dry hot climate and fresh to brackish water environment indicated by values of Sr/Cu, Sr/Ba and Mn/Fe ratios, which vary segment by segment. There are also similar variety regularities shown, which implicate that, the changes of paleoclimate influenced directly water salinity in the study area.</abstract><cop>Tallinn</cop><pub>Estonian Academy Publishers</pub><doi>10.3176/oil.2014.1.03</doi><tpages>1</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Basins Brackish Brackish water Climate Deposition Drying Freshwater Geological research Lithology Mineralization Mountains Oil shale Oil-shales Paleoclimatology Properties Saline water Salinity Sedimentation Segments Strontium Trace elements |
title | FORMATION CONDITIONS OF JIMUSAER OIL SHALE AT THE NORTHERN FOOT OF BOGDA MOUNTAIN, CHINA |
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