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- W2368704792 abstract "Its ordinary that parts of a suture zone is coverd with kinds of basins accompanying by its evolution in all orogenic belts. Premayily, these covering basins are divided into two kinds.One is longitudinal covering basins, overlapping but not destructuring the belt. Another is transversal destructive basins, not only covering but also destructuring the zone. Sysmetrical marine Jurassic basins is actually intracontinental subduction marginal foreland basins interrelated with the evolution of the Kongkala Wunquan Lancang River zone. Prospecting data probe that the belt is under the covering layers. plate tectonics formations in the two sides of the zone are different obviously and respectively belong to two kinds of continental margin. Thus it is concluded that the zone lies under the covering layers and presents three identification indicators of suture zone. [" @default.
- W2368704792 created "2016-06-24" @default.
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- W2368704792 date "2000-01-01" @default.
- W2368704792 modified "2023-09-24" @default.
- W2368704792 title "IDENTIFICATION INDICATORS OF KONGKALA-WUNQUAN-LANCANG RIVER SUTURE ZONE IN JURASSIC COVERING AREA IN TANGGULA MOUNTAINS" @default.
- W2368704792 hasPublicationYear "2000" @default.
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