Aulacogen Formation in Response to Opening the Ailaoshan Ocean: Origin of the Qin-Fang Trough, South...
Aulacogen Formation in Response to Opening the Ailaoshan Ocean: Origin of the Qin-Fang Trough, South China
About this item
Full title
Author / Creator
Publisher
Chicago: University of Chicago Press
Journal title
Language
English
Formats
Publication information
Publisher
Chicago: University of Chicago Press
Subjects
More information
Scope and Contents
Contents
The Qin-Fang Trough, South China, trends northeast-southwest, orthogonal to the adjoining southern margin of the craton. The Devonian strata within the trough are unconformable on late Neoproterozoic units of the Yunkai Massif, indicating that strata within the trough are autochthonous. U-Pb ages and Hf isotope compositions of detrital zircons from...
Alternative Titles
Full title
Aulacogen Formation in Response to Opening the Ailaoshan Ocean: Origin of the Qin-Fang Trough, South China
Authors, Artists and Contributors
Author / Creator
Identifiers
Primary Identifiers
Record Identifier
TN_cdi_jstor_primary_26547020
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_jstor_primary_26547020
Other Identifiers
ISSN
0022-1376
E-ISSN
1537-5269
DOI
10.1086/693036
