中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Contribution of high-pressure and ultrahigh-pressure rocks to the Jurassic sedimentation in Hefei basin

文献类型:期刊论文

作者Li, RW; Sun, S; Li, Z; Jiang, MS; Jin, FQ; Li, SY
刊名ACTA PETROLOGICA SINICA
出版日期2002-10-01
卷号18期号:4页码:526-530
关键词phengite high pressure and ultrahigh pressure rocks source rock Jurassic Hefei Basin
ISSN号1000-0569
文献子类Article
英文摘要The Jurassic sedimentary strata of Hefei Basin include the formations of Fanghushan, Sanjianpu, Zhougongshan and Fenghuangtai. Detrital white mica ubiquitously occurs in sandstones of these formations. The white mica is almost phengitic and the majority of the phengites has high Si content from 3.3 to 1 6 (P. f. u.), which indicates that the high-pressure and ultrahigh-pressure rocks were an important source for the Jurassic sediments of Hefei Basin. The Fanghushan Formation deposited during the early Jurassic. Therefore, the new discovery of detrital phengites in the Fanghushan Formation indicates that the high-pressure and ultrahigh-pressure rocks of the Dabie orogenic belt were already exposed to the surface in the early Jurassic time.
WOS关键词CENTRAL CHINA ; PROVENANCE ; ASSEMBLAGE ; MOUNTAINS
WOS研究方向Geology
语种英语
WOS记录号WOS:000179484500011
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/77679]  
专题中国科学院地质与地球物理研究所
通讯作者Li, RW
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Hefei Ind Univ, Dept Resource & Environm Sci, Hefei 230026, Peoples R China
推荐引用方式
GB/T 7714
Li, RW,Sun, S,Li, Z,et al. Contribution of high-pressure and ultrahigh-pressure rocks to the Jurassic sedimentation in Hefei basin[J]. ACTA PETROLOGICA SINICA,2002,18(4):526-530.
APA Li, RW,Sun, S,Li, Z,Jiang, MS,Jin, FQ,&Li, SY.(2002).Contribution of high-pressure and ultrahigh-pressure rocks to the Jurassic sedimentation in Hefei basin.ACTA PETROLOGICA SINICA,18(4),526-530.
MLA Li, RW,et al."Contribution of high-pressure and ultrahigh-pressure rocks to the Jurassic sedimentation in Hefei basin".ACTA PETROLOGICA SINICA 18.4(2002):526-530.

入库方式: OAI收割

来源:地质与地球物理研究所

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