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- W2355357260 abstract "On the basis of the different kinematic parameters, the major factors controlling heatanomaly during 0~40 Ma after collision were modelled. The results indicated the formationof heat anomaly with 250~900 km width of the orogenic belt were mainly controlled by adiabatic heating and viscous strain heating of the thickened lithosphere, not by heating derivedfrom radiogenic, the scratching of faults and magmatic intrusion. It is considered that the results could successfully explain the geochemical and gcophysical data in the northern-centralTibet Plateau." @default.
- W2355357260 created "2016-06-24" @default.
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- W2355357260 date "1998-01-01" @default.
- W2355357260 modified "2023-09-23" @default.
- W2355357260 title "MAJOR FACTORS CONTROLLING FORMATION OF HEAT ANOMALY IN COLLISION BELT" @default.
- W2355357260 hasPublicationYear "1998" @default.
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