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Sinistral to Normal Faulting along the Tan‐Lu Fault Zone: Evidence for Geodynamic Switching of the E...

Sinistral to Normal Faulting along the Tan‐Lu Fault Zone: Evidence for Geodynamic Switching of the E...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_jstor_primary_10_1086_651540

Sinistral to Normal Faulting along the Tan‐Lu Fault Zone: Evidence for Geodynamic Switching of the East China Continental Margin

About this item

Full title

Sinistral to Normal Faulting along the Tan‐Lu Fault Zone: Evidence for Geodynamic Switching of the East China Continental Margin

Publisher

Chicago: The University of Chicago Press

Journal title

The Journal of geology, 2010-05, Vol.118 (3), p.277-293

Language

English

Formats

Publication information

Publisher

Chicago: The University of Chicago Press

More information

Scope and Contents

Contents

The Tan‐Lu fault zone (TLFZ) along the East China continental margin (ECCM) experienced a change from sinistral to normal faulting in the late Mesozoic. Thirty‐four laser ablation (LA)‐ICPMS zircon U‐Pb dates for plutons and volcanic rocks along the TLFZ indicate that extension‐related magmatism started as early as 136 Ma. The development of pre‐er...

Alternative Titles

Full title

Sinistral to Normal Faulting along the Tan‐Lu Fault Zone: Evidence for Geodynamic Switching of the East China Continental Margin

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_jstor_primary_10_1086_651540

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_jstor_primary_10_1086_651540

Other Identifiers

ISSN

0022-1376

E-ISSN

1537-5269

DOI

10.1086/651540

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