- 责任者：Tang Jing (College of Earth Sciences ; Chengdu University of Technology ; Chengdu 610059 ; China) ; Zhu Lidong
- 刊名：Sedimentary Geology and Tethyan Geology
- 出版年：2013
- 卷期：33(1)
- 关键词：烃源岩 ; source rocks ; 青藏高原 ; Qinghai-Tibetan Plateau
- 页码：p.86-92
- 图表：illus., 3 tables, 15 refs.
- 分类号：1003
- issnNo：ISSN1009-3850
- isbnNo：CN51-1593/P
The source rocks consist of black oil shales, results of assessment of the from the Quse Formation in southern Qiangtang Basin on the Qinghai-Xizang dark grey argillutites and dark grey marls, with a total thickness of about 215.8 source rocks indicate that the organic matter abundances are higher, including Plateau m.The 9.23% for black oil shales, 2.21% for dark grey argillutites and 4.33% for dark grey marls, respectively. The organic matter types are classified into the type II for the argillutites, and dominantly the type II and subordinately the type III for the oil shales and marls. The pale brown colour for the kerogens and higher Tmax values （430℃ - 470℃ ） for the collected samples suggest the source rocks from the Quse Formation have reached up to the mature stage.