• The Core Journal of China
  • Included in Chinese Scientific and Technical Papers and Citations Database
  • Included in Chinese Science Citation Database (CSCD)
  • Included in Chemical Abstracts (CA)
  • Included in Scopus
Advanced Search
Liu Wanzhu, Du Xiaodi, Wang Pujun, Kuang Lichun, Wang Dongpo. A UNIQUE RESEARCH METHOD OF THE OUTCROP SEQUENCE STRATIGRAPHY: AN EXAMPLE FROM THE SILURIAN SECTION IN YINGAN VILLAGE,KEPING,XINJIANG[J]. Sedimentary Geology and Tethyan Geology, 1995, 15(5): 29-32.
Citation: Liu Wanzhu, Du Xiaodi, Wang Pujun, Kuang Lichun, Wang Dongpo. A UNIQUE RESEARCH METHOD OF THE OUTCROP SEQUENCE STRATIGRAPHY: AN EXAMPLE FROM THE SILURIAN SECTION IN YINGAN VILLAGE,KEPING,XINJIANG[J]. Sedimentary Geology and Tethyan Geology, 1995, 15(5): 29-32.

A UNIQUE RESEARCH METHOD OF THE OUTCROP SEQUENCE STRATIGRAPHY: AN EXAMPLE FROM THE SILURIAN SECTION IN YINGAN VILLAGE,KEPING,XINJIANG

More Information
  • Received Date: March 16, 1995
  • Published Date: October 29, 1995
  • Sequence stratigraphic principles can be applied to the study of all the outcrops,espe-cially those near the depositional shoreline break where the sea-level changes can be sensi-tively recorded.In this paper,the authors have summarized a unique method,i,e."laterally tracing,multiouterop correlation and regionally detailed mapping" which is especially appli-cable to the spot outcrop study.As an example of this method,the Silurian outcrops from Yingan Village,Keping,Xinjiang are described,and the results of the study of sea-level changes are also presented.
  • Related Articles

    [1]CHENG Jinxiang, DENG Min, YANG Guilai, YU Qian. Analysis of geochemical characteristics, provenance, and tectonic background of black shale in the Silurian Longmaxi Formation of the Mingsheng section in the Yanyuan area, Sichuan Province[J]. Sedimentary Geology and Tethyan Geology, 2024, 44(4): 840-853. DOI: 10.19826/j.cnki.1009-3850.2023.12003
    [2]SHANG Kai, GUO Na, ZHANG Rui. Sedimentary facies of the lower bitumen-bearing sandstone member of the Silurian Kepingtage Formation in the S1 well area, Tarim Basin[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(4): 14-20.
    [3]MIAO Qing, FU Heng. Sequence stratigraphy of the Silurician strata in the northern and central Tarim Basin[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(1): 34-41.
    [4]HOU Gang-fu, WANG Hai-yan, ZHANG Xian-long, SUN Xiong-wei, ZENG Qing-lu. Development and distribution of the Silurian reservoir-seal associations in the Tarim Basin, Xinjiang[J]. Sedimentary Geology and Tethyan Geology, 2012, 32(2): 59-65.
    [5]ZHAO Wen-guang, PENG Shi-mi, CAI Zhong-xian, HAN Tao. Sequence stratigraphy of the Silurian strata and accommodation spaces in central Tarim Basin,Xinjiang[J]. Sedimentary Geology and Tethyan Geology, 2006, 26(4): 51-56.
    [6]WU Yao-dong, JIANG Lai-li, CHU Dong-ru, Wu Wei-ping, WU Hai-quan, WANG De-hua. Sequence stratigraphy of the Nanhuan-Silurian strata in Southwest Anhui[J]. Sedimentary Geology and Tethyan Geology, 2003, 23(1): 45-52.
    [7]LI Zhong-xiong, QIAN Yong-zhen. Recent progress in the research on the Sinian conodonts from the western margin of the Yangtze platform[J]. Sedimentary Geology and Tethyan Geology, 2001, 21(3): 87-101.
    [8]ZOU Guang-fu, CHEN Yong-ming. Silurian sequence stratigraphy of the western margin of the Yangtze platform in China[J]. Sedimentary Geology and Tethyan Geology, 2000, 20(3): 48-53.
    [9]HE Yuan-xiang, QIAN Yong-zhen. The Silurian-Devonian boundary in Baizitian, Yanbian, Sichuan and its geological implications[J]. Sedimentary Geology and Tethyan Geology, 2000, 20(1): 98-112.
    [10]Zhang Tingshan, Yu Jianhua, Bian Lizeng, S. Kershaw, Chen Xiaohui, Lan Guangzhi, Wan Yun. Strontium,carbon and oxygen isotopic compositions and their geological significance:the Silurian strata on the northern and southern margins of the Sichuan Basin[J]. Sedimentary Geology and Tethyan Geology, 1998, 18(3): 41-49.

Catalog

    Article views (69) PDF downloads (51) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return