Flake tectonics in the Sulu orogen in eastern China as revealed by seismic tomography

被引：45

作者：

Xu, PF ^{[1
]}

Liu, FT ^{[1
]}

Ye, K ^{[1
]}

Wang, QC ^{[1
]}

Cong, BL ^{[1
]}

Chen, H ^{[1
]}

机构：

[1] Chinese Acad Sci, Inst Geol & Geophys, Beijing 100101, Peoples R China

来源：

GEOPHYSICAL RESEARCH LETTERS | 2002年 / 29卷 / 10期

关键词：

D O I：

10.1029/2001GL014185

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

[1] Seismic tomographic image reveals a crocodile-like P-waves velocity structure beneath the Sulu orogenic belt, which marks the subduction/collision zone between the Sino-Korean block (SK) and Yangtze block (YZ) in eastern China. It may imply that the upper crust of the YZ was detached from its lower crust and thrust over the SK for a maximum of similar to400 km in the Sulu region, whereas the remnant of the subducted Yangtze lithosphere was lay beneath the SK. This crustal detached structure (flake tectonics) might have occurred after the Triassic subduction/collision.

引用

页码：23 / 1

页数：4

共 30 条

[1]

Chen H., 1988, oil & gas geol., V33, P211

[2] Trace element and isotope characteristics of Cenozoic basalts around the Tanlu fault with implications for the eastern plate boundary between North and South China [J].

Chung, SL .

JOURNAL OF GEOLOGY, 1999, 107 (03) :301-312

[3]

CONG B, 1995, EUR J MINERAL, V7, P119

[4]

Cong B.L., 1996, ULTRAHIGH PRESSURE M

[5]

LI ZX, 1994, GEOLOGY, V22, P739, DOI 10.1130/0091-7613(1994)022<0739:CBTNAS>2.3.CO

[6]

[7]

LIN W, 2002, IN PRESS SCI GEOLOGI

[8]

LIU F, 1984, J GEOPHYS, V27, P167

[9]

LIU FT, 1990, GEOPHYS J INT, V101, P379, DOI 10.1111/j.1365-246X.1990.tb06576.x

[10] Mineral inclusions in zircon from gneisses in the ultrahigh-pressure zone of the Dabie Mountains, China [J].

Liu, JB ;

Ye, K ;

Maruyama, SN ;

Cong, BL ;

Fan, HR .

JOURNAL OF GEOLOGY, 2001, 109 (04) :523-535

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