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Evolution of calc-alkaline to alkaline magmatism through Carboniferous convergence to Permian transc...

Evolution of calc-alkaline to alkaline magmatism through Carboniferous convergence to Permian transc...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_21200138

Evolution of calc-alkaline to alkaline magmatism through Carboniferous convergence to Permian transcurrent tectonics, western Chinese Tianshan

About this item

Full title

Evolution of calc-alkaline to alkaline magmatism through Carboniferous convergence to Permian transcurrent tectonics, western Chinese Tianshan

Publisher

Berlin/Heidelberg: Springer-Verlag

Journal title

International journal of earth sciences : Geologische Rundschau, 2009-09, Vol.98 (6), p.1275-1298

Language

English

Formats

Publication information

Publisher

Berlin/Heidelberg: Springer-Verlag

More information

Scope and Contents

Contents

Continuous magmatic activity occurred in the western Chinese Tianshan, Central Asia, from the Carboniferous to the Permian, i.e. before and after the Late Carboniferous amalgamation of Junggar and the Yili Blocks. Zircon U–Pb LA-ICPMS and Ar–Ar data reveal a coincidence in time between regional wrench faulting and granitoid emplacement. Permian pos...

Alternative Titles

Full title

Evolution of calc-alkaline to alkaline magmatism through Carboniferous convergence to Permian transcurrent tectonics, western Chinese Tianshan

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_miscellaneous_21200138

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_21200138

Other Identifiers

ISSN

1437-3254

E-ISSN

1437-3262

DOI

10.1007/s00531-008-0408-y

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