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晚奥陶世五峰期扬子海盆海平面变化旋回与古水体深度

何卫红 汪啸风 卜建军

何卫红, 汪啸风, 卜建军. 晚奥陶世五峰期扬子海盆海平面变化旋回与古水体深度[J]. 沉积学报, 2002, 20(3): 367-375.
引用本文: 何卫红, 汪啸风, 卜建军. 晚奥陶世五峰期扬子海盆海平面变化旋回与古水体深度[J]. 沉积学报, 2002, 20(3): 367-375.
HE Wei-hong, WANG Xiao-feng, BU Jian-jun. The Eustatic Cycles and the Depth of Water Mass of the Latest Ordovician Wufengian in the Yangtse Basin[J]. Acta Sedimentologica Sinica, 2002, 20(3): 367-375.
Citation: HE Wei-hong, WANG Xiao-feng, BU Jian-jun. The Eustatic Cycles and the Depth of Water Mass of the Latest Ordovician Wufengian in the Yangtse Basin[J]. Acta Sedimentologica Sinica, 2002, 20(3): 367-375.

晚奥陶世五峰期扬子海盆海平面变化旋回与古水体深度

基金项目: 中国地质调查局所支持的研究项目“震口系及显生宙年代地层划分的界线标志和时限的研究”的成果的一部分
详细信息
    作者简介:

    何卫红,女, 1972年出生,硕士研究生,地层古生物学,综合地层学

  • 中图分类号: P534.42;P531

The Eustatic Cycles and the Depth of Water Mass of the Latest Ordovician Wufengian in the Yangtse Basin

  • 摘要: 通过晚奥陶世五峰期扬子海盆的古地理格局、岩性及生物群的纵向变化、Ce异常变化的旋回性和生物群对海水深度的指示作用的讨论, 认为扬子海盆晚奥陶世五峰期经历了5个旋回的海平面变化, 海水最浅为 50~ 80m(观音桥层 ), 海水最深约500m左右。
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  • 收稿日期:  2001-08-09
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目录

    晚奥陶世五峰期扬子海盆海平面变化旋回与古水体深度

      基金项目:  中国地质调查局所支持的研究项目“震口系及显生宙年代地层划分的界线标志和时限的研究”的成果的一部分
      作者简介:

      何卫红,女, 1972年出生,硕士研究生,地层古生物学,综合地层学

    • 中图分类号: P534.42;P531

    摘要: 通过晚奥陶世五峰期扬子海盆的古地理格局、岩性及生物群的纵向变化、Ce异常变化的旋回性和生物群对海水深度的指示作用的讨论, 认为扬子海盆晚奥陶世五峰期经历了5个旋回的海平面变化, 海水最浅为 50~ 80m(观音桥层 ), 海水最深约500m左右。

    English Abstract

    何卫红, 汪啸风, 卜建军. 晚奥陶世五峰期扬子海盆海平面变化旋回与古水体深度[J]. 沉积学报, 2002, 20(3): 367-375.
    引用本文: 何卫红, 汪啸风, 卜建军. 晚奥陶世五峰期扬子海盆海平面变化旋回与古水体深度[J]. 沉积学报, 2002, 20(3): 367-375.
    HE Wei-hong, WANG Xiao-feng, BU Jian-jun. The Eustatic Cycles and the Depth of Water Mass of the Latest Ordovician Wufengian in the Yangtse Basin[J]. Acta Sedimentologica Sinica, 2002, 20(3): 367-375.
    Citation: HE Wei-hong, WANG Xiao-feng, BU Jian-jun. The Eustatic Cycles and the Depth of Water Mass of the Latest Ordovician Wufengian in the Yangtse Basin[J]. Acta Sedimentologica Sinica, 2002, 20(3): 367-375.
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