Test of Deep Seismic Reflection Profiling across Central Uplift of Qiangtang Terrane in Tibetan Plateau

A test of deep seismic reflection profiling across the central uplift or metamorphic belt of the Qiangtang （羌塘） terrane, Tibet plateau, provides a first image of the crustal structure. Complex reflection patterns in the upper crust are interpreted as a series of folds and thrusts, and bivergent refl...

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Bibliographic Details
Published inJournal of earth science (Wuhan, China) Vol. 20; no. 2; pp. 438 - 447
Main Author 卢占武 高锐 李秋生 贺日政 匡朝阳 侯贺晟 熊小松 管烨 王海燕 Klemperer S L
Format Journal Article
LanguageEnglish
Published China University of Geosciences (Wuhan) China University of Geosciences (Wuhan) 01.04.2009
Springer Nature B.V
Subjects
Biogeosciences
Earth and Environmental Science
Earth science
Earth Sciences
Geochemistry
Geology
Geotechnical Engineering & Applied Earth Sciences
Metamorphic rocks
Plate tectonics
Seismology
中央
反射模式
地壳结构
深地震反射剖面
羌塘地体
西藏高原
试验
隆起
crustal structure
Qiangtang terrane
test of deep reflection profiling
central uplift zone
convergent process
Online AccessGet full text
ISSN1674-487X
1867-111X
DOI10.1007/s12583-009-0036-x

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Summary:A test of deep seismic reflection profiling across the central uplift or metamorphic belt of the Qiangtang （羌塘） terrane, Tibet plateau, provides a first image of the crustal structure. Complex reflection patterns in the upper crust are interpreted as a series of folds and thrusts, and bivergent reflections in the lower crust may represent a convergence between the Indian and the Eurasian plates.
Bibliography:P315.2
P548
Qiangtang terrane, central uplift zone, crustal structure, test of deep reflection profiling,convergent process.
42-1788/P
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ISSN:1674-487X
1867-111X
DOI:10.1007/s12583-009-0036-x