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欧亚大陆北部盆地发育历史——来自东西向跨洲剖面的证据

毛翔 李江海 傅臣建 程海艳 高危言

地质科学Issue(3):763-774,12.
地质科学Issue(3):763-774,12.

欧亚大陆北部盆地发育历史——来自东西向跨洲剖面的证据

Developments of basins in northern Eurasia:Evidence from E-W inter-continent profile

毛翔 1李江海 1傅臣建 1程海艳 1高危言1

作者信息

  • 1. 造山带与地壳演化教育部重点实验室,北京大学地球与空间科学学院 北京 100871
  • 折叠

摘要

Abstract

Plates' evolution controls the forming and developing of basins, and the natures and geological characteristics of basins are determined by the tectonic units. This thesis is focused on analysis of geotectonic backgrounds and draws an 11 000-km-long Eurasia east-west trending intra-continent profile ( along N60° ±5°, from Lough Neagh Arran Basin in the North Sea to North Okhotsk Basin). The profile divides tectonic units into different levels ( supercontinent and tectonic domain, plate and orogeny, block and tectonic belt, basin and arch ) and links tectonic events and different levels of units to reveals the structure of the most upper crust (less than 12 km depth) related to the regional tectonics in the northern Eurasia continent. The profile traverses the Atlantic extensional boundary and the Pacific subducting boundary, crosses 12 basins,Siberian Craton and Tatar Strait-Sakhalin Island-The Okhotsk Sea,etc.,involving all kinds of basins in Wilson cycle. The most important effect of the profile is that it associates plate boundary with the inside of the basin since it leads to the possibility of contrasting different basins' evolutions.

关键词

欧亚大陆/剖面/盆地结构/构造演化

Key words

Eurasia/Profile/Basins/Tectonic evolution

分类

天文与地球科学

引用本文复制引用

毛翔,李江海,傅臣建,程海艳,高危言..欧亚大陆北部盆地发育历史——来自东西向跨洲剖面的证据[J].地质科学,2011,(3):763-774,12.

基金项目

国家重点基础研究发展计划“973”项目(编号:2009CB219302)资助. (编号:2009CB219302)

地质科学

OA北大核心CSCDCSTPCD

0563-5020

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