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Dube Dube (1970)
Upper mantle structure in and around the Indian subcontinent (from S‐wave)Indian J. Met. Geophys, 21
Kaila Kaila (1978)
Structure of the Kashmir from deep seismic soundingJournal of the Geological Society of India, 19
Rui Rui, Jieshou Jieshou, Ding Ding, Chen Chen, He He, Yang Yang, Zhou Zhou, Sun Sun (1981)
Crustal structure in China from surface wavesActa Seismologica, 3
Guodong Guodong, Qun Qun, Shi Shi, Sun Sun, Shi Shi, Liu Liu (1983)
The electrical structure of the crust and upper mantle and its relationship with seismicity in the Beijing‐Tianjin‐Tangshan region and adjacent areaActa Geophysica Sinica, 26
Abstract Through recent study, the author considers that the north‐south‐trending Kangding‐Honghe tectonic belt is not a marginal uplift zone of the Yangtze Platform but a Te thy an‐type collisional tectonic belt of which the crust‐upper mantle can be structurally divided into three layers. The upper layer is the brittle upper crust, dominated by overthrusting and imbrication; the middle layer is the plastic lower crust and part of the upper mantle, represented by compression and shortening; and the lower layer is the upper, mantle, probably belonging to the Yangtze Platform in light of the thickness of the lithosphere.
Acta Geologica Sinica (English Edition) – Wiley
Published: Sep 1, 1989
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