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渭河盆地中部区域地壳形变及应变的分布特征

瞿伟 王庆良 张勤 张明

大地测量与地球动力学2012,Vol.32Issue(4):33-36,4.
大地测量与地球动力学2012,Vol.32Issue(4):33-36,4.

渭河盆地中部区域地壳形变及应变的分布特征

ON CRUSTAL DEFORMATION-STRAIN CHARACTERISTICS OF CENTRAL REGION OF WEIHE BASIN

瞿伟 1王庆良 2张勤 3张明1

作者信息

  • 1. 长安大学地质工程与测绘学院,西安710054
  • 2. 西部矿产资源与地质工程教育部重点实验室,西安710054
  • 3. 中国地震局第二监测中心,西安710054
  • 折叠

摘要

Abstract

On the basis of the "digital seismic network engineering" GPS monitoring results, and combined with regional tectonic features,the 2D finite element model of the Weihe basin central region is built. According to the above, the present crustal deformation-strain distribution characteristics of the studied area are obtained. The results show that the Xi' an-Xianyang area is of significantly high value of the surface expansion and mainly tensile strain within the area, the value respectively reaches more than 2. 0 × 10-6 /a and 3.5×10-6/a. Thus the present crustal tensile tectonic activity of Xi' an-Xianyang area is strong.

关键词

渭河盆地中部/有限元/地壳形变/应变特征/地裂缝

Key words

Weihe basin central region/ finite element model/ crustal deformation/ strain feature / ground fissures

分类

天文与地球科学

引用本文复制引用

瞿伟,王庆良,张勤,张明..渭河盆地中部区域地壳形变及应变的分布特征[J].大地测量与地球动力学,2012,32(4):33-36,4.

基金项目

国家自然科学基金重点项目(41130753) (41130753)

国家自然科学基金(41072266,41104019) (41072266,41104019)

国土资源大调查项目(1212010914015) (1212010914015)

大地测量与地球动力学

OA北大核心CSCDCSTPCD

1671-5942

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