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《Earth Science Frontiers》 2003-S1
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CONTINENTAL LITHOSPHERE DECOUPLING:IMPLICATION FOR BLOCK MOVEMENT

YANG Xiao-song, MA Jin (Laboratory of Earthquake Dynamics, Institute of Geology, China Seismological Bureau, Beijing 100029, China)  
It is necessary to determine the petrophysical features of the weak layers of underlain blocks for identifying them by geophysical surveys and for understanding the block movement. However, we have little knowledge about the nature and structural features of the layers to date. On the basis of the data of modern petrological and petrophysical experiments, geophysical surveys and geological investigations, the authors have discussed the petrophysical characteristics of the layers. Blocks can be divided into two typical kinds—the crustal block and the lithospheric block. The former is the “thin plate” constituted by the upper part of crust that lies on an intracrustal weak layer or potential decoupling zone along which the crustal block can move independently to some extent. The latter is mechanically coupled in lithosphere scale, and consequently it lies on asthenosphere and the top of asthenosphere is regarded as its bottom. The distinguishable features of the intracrustal weak zone are both low velocity when seismic waves pass though the layer perpendicularly and anisotropy. Therefore, it is expected to detect the zone by multi-seismic methods. Generally, in active tectonic regions, intracrustal partial melting zone is one of candidates to cause the upper part of crust (crustal block) to decouple to the other part of lithosphere. The low velocity zones attributed to partial melting occur within the depth of 20~35 km in southern Tibet and Sichuan-Yunnan extensively. The blocks in these areas are partially decoupling along the low velocity zones.
【Fund】: 国家重点基础研究发展规划项目 (G19980 40 70 0 ) ;; 国家自然科学基金资助项目 (4 0 0 72 0 62 ) ;; 地震科学联合基金项目
【CateGory Index】: P313
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