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琼东南盆地岩石圈伸展模拟探讨——以测线1为例

贺超 吴世敏 龙根元

海洋地质前沿2017,Vol.33Issue(8):24-31,8.
海洋地质前沿2017,Vol.33Issue(8):24-31,8.DOI:10.16028/j.1009-2722.2017.08004

琼东南盆地岩石圈伸展模拟探讨——以测线1为例

LITHOSPHERIC STRETCHING MODELING OF QIONGDONGNAN BASIN:BASED ON LINE 1

贺超 1吴世敏 2龙根元1

作者信息

  • 1. 海南省海洋地质调查研究院,海口570206
  • 2. 中山大学地球科学与工程学院,广州510275
  • 折叠

摘要

Abstract

In order to better understand the lithospheric extension process of the Qiongdongnan Basin,lithospheric stretching factors were calculated along the Line 1 which across both the continental shelf and slope.Upper-crust stretching factors were calculated by summing heaves measured on seismically imaged faults,varying from 1.678~2.238.Whole crust stretching factors changed from 1.251 ~ 2.468,derived from crustal-thinning constrained by seismic reflection and gravity inversion.Lithosphere stretching factors were determined from the combination of the two-dimensional flexural-cantilever forward and reverse modeling,ranging from 1.062~2.647.The results indicate that the depth dependent model is likely optional in the Qiongdongnan Basin.But the stretch factors are not simply increasing with depth,but also related to rheological features and the anisotropy of lithosphere before stretching.

关键词

伸展因子/二维正反演模拟/琼东南盆地

Key words

stretching factor β/2D forward and reverse modeling/Qiongdongnan Basin

分类

海洋科学

引用本文复制引用

贺超,吴世敏,龙根元..琼东南盆地岩石圈伸展模拟探讨——以测线1为例[J].海洋地质前沿,2017,33(8):24-31,8.

基金项目

国家自然科学基金(41276048,91328205,41476039) (41276048,91328205,41476039)

海洋地质前沿

OACSCDCSTPCD

1009-2722

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