Oil shale formation in the Upper Cretaceous Nenjiang Formation of the;Songliao Basin (NE China): Implications from organic and inorganic;geochemical analyses
Jia, Jianliang2; Bechtel, Achim; Liu, Zhaojun2; Strobl, Susanne A. I.; Sun, Pingchang2; Sachsenhofer, Reinhard F.
刊名INTERNATIONAL JOURNAL OF COAL GEOLOGY
2013
卷号113页码:11-26
ISSN号0166-5162
DOI10.1016/j.coal.2013.03.004
英文摘要Two oil shale layers are present in the Upper Cretaceous Nenjiang Formation of the Songliao Basin, representing excellent hydrocarbon source rocks. Their biomarker compositions provide evidence for a major contribution by aquatic organisms within the photic zone of the water column. Phytoplankton blooms were promoted by warm-humid climate, and lake eutrophication. Salinity stratification and anoxic bottom water conditions are indicated in the lower oil shale layer, whereas decreased salinity and partial oxygenation of the water column are evident in the upper oil shale layer. Moreover, an increase in sizes of alginite from the lower to the upper oil shale layer and enhanced telalginite concentrations is detected. Therefore, a stratified water column with high salinity and anoxic bottom water conditions contributes to organic matter (OM) preservation in the lower oil shale layer. In contrast, high bioproductivity in combination with OM preservation favored by enhanced algae sizes and telalginite concentrations are suggested as the OM enrichment mechanisms in the upper oil shale layer. In addition, factors such as clay minerals, microbial activity, and detrital matter input cannot be ignored for their influence on OM enrichment.;In this study, a preservation model within the lower oil shale layer and a productivity model within the upper oil shale layer are established. The models imply that excellent preservation is the major controlling factor for OM enrichment in the lower oil shale layer, whereas the high bioproductivity is the major controlling factor for OM enrichment in the upper oil shale layer. However, the combination of both factors for oil shale deposition must be considered. Crown Copyright (C) 2013 Published by Elsevier B.V. All rights reserved.
学科主题油气地质
WOS关键词LACUSTRINE SOURCE ROCKS ; ISOTOPE GEOCHEMISTRY ; SEDIMENTARY RECORD ; NORTHEAST CHINA ; CLIMATIC-CHANGE ; SOUTHERN CHINA ; VIKING GRABEN ; GREAT-PLAINS ; GOSAU GROUP ; CARBON
WOS研究方向Energy & Fuels ; Geology
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000320496900002
内容类型期刊论文
源URL[http://119.78.100.197/handle/2HKVOGP0/40191]  
专题中国地质科学院地质研究所
作者单位1.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China.
2.Jia, Jianliang; Bechtel, Achim; Strobl, Susanne A. I.; Sachsenhofer, Reinhard F.] Univ Leoben, Dept Appl Geosci & Geophys, A-8700 Leoben, Austria.
3.Jilin Univ, Coll Earth Sci, Changchun 130061, Peoples R China.
推荐引用方式
GB/T 7714
Jia, Jianliang,Bechtel, Achim,Liu, Zhaojun,et al. Oil shale formation in the Upper Cretaceous Nenjiang Formation of the;Songliao Basin (NE China): Implications from organic and inorganic;geochemical analyses[J]. INTERNATIONAL JOURNAL OF COAL GEOLOGY,2013,113:11-26.
APA Jia, Jianliang,Bechtel, Achim,Liu, Zhaojun,Strobl, Susanne A. I.,Sun, Pingchang,&Sachsenhofer, Reinhard F..(2013).Oil shale formation in the Upper Cretaceous Nenjiang Formation of the;Songliao Basin (NE China): Implications from organic and inorganic;geochemical analyses.INTERNATIONAL JOURNAL OF COAL GEOLOGY,113,11-26.
MLA Jia, Jianliang,et al."Oil shale formation in the Upper Cretaceous Nenjiang Formation of the;Songliao Basin (NE China): Implications from organic and inorganic;geochemical analyses".INTERNATIONAL JOURNAL OF COAL GEOLOGY 113(2013):11-26.
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