Remelting of subducted continental lithosphere: Petrogenesis of Mesozoic magmatic rocks in the Dabie...
Remelting of subducted continental lithosphere: Petrogenesis of Mesozoic magmatic rocks in the Dabie-Sulu orogenic belt
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Publisher
Heidelberg: SP Science in China Press
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Language
English
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Publisher
Heidelberg: SP Science in China Press
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Contents
The Dabie-Sulu orogenic belt was formed by the Triassic continental collision between the South China Block and the North China Block. There is a large area of Mesozoic magmatic rocks along this orogenic belt, with emplacement ages mainly at Late Triassic, Late Jurassic and Early Cretaceous. The Late Triassic alkaline rocks and the Late Jurassic gr...
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Full title
Remelting of subducted continental lithosphere: Petrogenesis of Mesozoic magmatic rocks in the Dabie-Sulu orogenic belt
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Record Identifier
TN_cdi_proquest_journals_209790883
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_209790883
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ISSN
1674-7313,1006-9313
E-ISSN
1869-1897,1862-2801
DOI
10.1007/s11430-009-0134-8
