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关于红海裂谷盆地的构造与沉积输入演化的研究综述

  • ABDUALLAH M. I. Mohamed ,
  • 刘堂晏
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  • 1. 同济大学 海洋与地球科学学院, 上海 200092, 中国
    2. 红海大学 地球科学学院, 苏丹港 33311, 苏丹

收稿日期: 2020-04-21

  网络出版日期: 2021-01-22

A review about tectonic and sedimentary input evolution of the Red Sea rifting basin

  • I. Mohamed ABDUALLAH M. ,
  • Tangyan LIU
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  • 1. School of Marine and Earth Science, Tongji University, Shanghai 200092, China
    2. Faculty of Earth Science, Red Sea University, Port Sudan 33311, Sudan

Received date: 2020-04-21

  Online published: 2021-01-22

摘要

盆地是一个沉降明显的地区, 在那里可以堆积沉积物. 红海盆地是一个体系的一部分, 其裂谷和胚胎海盆从东非延伸至黎凡特地区, 这是非洲-阿拉伯大陆早渐新世解体形成的. 它是世界上仅有的两个新生裂谷盆地之一, 另一个是伍德拉克盆地, 被认为是研究板块构造现象、沉积形成演化和气候变化的世界最佳自然实验室. 红海是一个年轻的海洋盆地, 从大陆裂谷发育到真正的海洋海底分散. 它包括世界上3.8%的珊瑚礁. 红海盆地的水与世界其他海洋相比是独一无二的, 没有河流流入. 由于缺乏河流输入和永久性河流, 陆源物质仅在暴雨和洪水暴发期间供应. 频繁的沙尘暴(风输送)和钙质生物粉土对海域的塑造很关键. 红海裂谷系统是世界上最大的动态断裂构造体系之一, 它是从最初的裂谷和断裂发展到大陆裂谷的几个阶段, 最后形成大洋板块. 它是监测威尔逊旋回现象的极好场所.

本文引用格式

ABDUALLAH M. I. Mohamed , 刘堂晏 . 关于红海裂谷盆地的构造与沉积输入演化的研究综述[J]. 华东师范大学学报(自然科学版), 2020 , 2020(S1) : 74 -78 . DOI: 10.3969/j.issn.1000-5641.202092201

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