Palaeoenvironment and organic matter of the Triassic Chang 9 lacustrine shales, Ordos Basin, China
文献类型：期刊论文
| 作者 | Xu, Zhengjian1,2,3,7; Liu, Luofu1,2; Jiang, Shu7,8; Wang, Tieguan1,2; Fang, Chao6; Zhang, Zhihuan1,2; Wu, Kangjun3; Feng, Yanjun5,7; Dou, Wenchao1,2,4 |
| 刊名 | GEOLOGICAL JOURNAL
 |
| 出版日期 | 2019-12-08 |
| 页码 | 24 |
| ISSN号 | 0072-1050 |
| 关键词 | biomarker element concentration lacustrine shales Ordos Basin organic matter source palaeoenvironment |
| DOI | 10.1002/gj.3706 |
| 英文摘要 | The Ordos Basin, a large mainly non-marine basin, is an important petroliferous basin in northern China. The Triassic Chang 9 shales, including the delta plain shale (DPS), delta front shale (DFS), and deep lake shale (DLS), are proven to be the main source rocks in the lower Yanchang Formation (LYF). This study investigates the source rock potential, palaeoenvironment, and organic matter (OM) source. According to the OM thermal maturity, abundance, and type, the shales have excellent source rock potential. The DLS has the highest quality with average TOC of 7.08%, S-1 + S-2 of 14.41 mg HC/g rock, and Type II1-II2. According to correlations of Rb/Sr versus Sr/Cu, the shales were mainly deposited in arid conditions. Based on the major element (S), trace elements (V, Ni, Co, Cr, U, and Th), rare earth element (Ce) concentrations, and biomarkers (Pr, Ph, dibenzofuran, fluorene, and dibenzothiophene), redox conditions for the DPS, DFS, and DLS were oxidizing, sub-oxidizing to sub-reducing, and reducing, respectively. The palaeosalinity was fresh- to brackish-water, ascertained by the trace elements (Sr and Ba) and biomarkers (gammacerane). The water stratification was controlled by the temperature changes and the palaeosalinity differences, and the maximum water depth was similar to 100 m during the Chang 9 deposition. Aquatic microorganisms (e.g., algae, bacteria, and phytoplankton) were the main organic matter sources for the shales, mixed together with terrigenous plants in DPS and DFS. The DLS has the most aquatic microorganisms and has the least higher plant fragments, supported by the higher TOC (up to 14%), lowest vitrinite contents (Avg. = 14.1%), and highest liptinite contents (Avg. = 59.5%). Laterally, the DPS, DFS, and DLS were distributed successively from the lake margin to the depocentre. Vertically, the DLS, DFS, and DPS were developed successively from the bottom lake to the upper lake. The DLS was mainly formed in an environment of high-level sapropelinite and favourable preservation conditions, and the DPS was mainly formed in an environment of high-level terrigenous inputs and poor preservation conditions, while the DFS was mainly formed in an environment of medium-level of sapropelinite productivity and terrigenous inputs and fair preservation conditions. The DPS and DFS were formed during both the early stage (shallow lake) and the late stage (deep lake) of the Chang 9 deposition, while the DLS was only developed in the deep lake during the late Chang 9 deposition. The high-level sapropelinite production and favourable preservation controlled the formation of the organic-rich shales, especially for the organic-rich DLS. |
| WOS关键词 | RARE-EARTH-ELEMENTS ; SOURCE ROCKS ; YANCHANG FORMATION ; RICH SHALES ; OIL-SHALE ; CRUDE OILS ; DEPOSITIONAL ENVIRONMENT ; TRACE-ELEMENTS ; SEDIMENTARY CHARACTERISTICS ; GEOCHEMICAL CHARACTERISTICS |
| 资助项目 | China Scholarship Council[201806440137] ; Research Fund for the Doctoral Program of Higher Education of China[20130007110002] ; Scientific and Technology Innovation Fund - Coal Mining Research Branch[KJ-2019-TDKCMS-03] ; National Natural Science Foundation of China[41372143] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| 出版者 | WILEY |
| WOS记录号 | WOS:000501460900001 |
| 资助机构 | China Scholarship Council ; China Scholarship Council ; Research Fund for the Doctoral Program of Higher Education of China ; Research Fund for the Doctoral Program of Higher Education of China ; Scientific and Technology Innovation Fund - Coal Mining Research Branch ; Scientific and Technology Innovation Fund - Coal Mining Research Branch ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Scholarship Council ; China Scholarship Council ; Research Fund for the Doctoral Program of Higher Education of China ; Research Fund for the Doctoral Program of Higher Education of China ; Scientific and Technology Innovation Fund - Coal Mining Research Branch ; Scientific and Technology Innovation Fund - Coal Mining Research Branch ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Scholarship Council ; China Scholarship Council ; Research Fund for the Doctoral Program of Higher Education of China ; Research Fund for the Doctoral Program of Higher Education of China ; Scientific and Technology Innovation Fund - Coal Mining Research Branch ; Scientific and Technology Innovation Fund - Coal Mining Research Branch ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Scholarship Council ; China Scholarship Council ; Research Fund for the Doctoral Program of Higher Education of China ; Research Fund for the Doctoral Program of Higher Education of China ; Scientific and Technology Innovation Fund - Coal Mining Research Branch ; Scientific and Technology Innovation Fund - Coal Mining Research Branch ; National Natural Science Foundation of China ; National Natural Science Foundation of China |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/95814]  |
| 专题 | 地质与地球物理研究所_其他部门 |
| 通讯作者 | Liu, Luofu; Jiang, Shu |
| 作者单位 | 1.China Univ Petr, State Key Lab Petr Resources & Prospecting, Beijing, Peoples R China 2.China Univ Petr, Coll Geosci, Beijing, Peoples R China 3.Chongqing Univ Sci & Technol, Sch Petr Engn, Chongqing, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China 5.China Coal Res Inst, Coal Min Res Branch, Beijing, Peoples R China 6.CNPC Engn Technol R&D Co Ltd, Drilling Technol Dept, Beijing, Peoples R China 7.Univ Utah, Energy & Geosci Inst, Salt Lake City, UT USA 8.China Univ Geosci, Fac Earth Resources, Key Lab Tecton & Petr Resources, Minist Educ, Wuhan, Hubei, Peoples R China |
| 推荐引用方式 GB/T 7714 | Xu, Zhengjian,Liu, Luofu,Jiang, Shu,et al. Palaeoenvironment and organic matter of the Triassic Chang 9 lacustrine shales, Ordos Basin, China[J]. GEOLOGICAL JOURNAL,2019:24. |
| APA | Xu, Zhengjian.,Liu, Luofu.,Jiang, Shu.,Wang, Tieguan.,Fang, Chao.,...&Dou, Wenchao.(2019).Palaeoenvironment and organic matter of the Triassic Chang 9 lacustrine shales, Ordos Basin, China.GEOLOGICAL JOURNAL,24. |
| MLA | Xu, Zhengjian,et al."Palaeoenvironment and organic matter of the Triassic Chang 9 lacustrine shales, Ordos Basin, China".GEOLOGICAL JOURNAL (2019):24. |
入库方式： OAI收割
来源：地质与地球物理研究所
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