Uniform postglacial slip-rate along the central 600 km of the Kunlun Fault (Tibet), from 26Al, 10Be, and 14C dating of riser offsets, and climatic origin of the regional morphology

Authors

J. Woerd

Published

March 27, 2002

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Journal

Geophysical Journal International

Topics

DOI

10.1046/j.1365-246x.2002.01556.x

Uniform postglacial slip-rate along the central 600 km of the Kunlun Fault (Tibet), from 26Al, 10Be, and 14C dating of riser offsets, and climatic origin of the regional morphology

Authors

J. Woerd

Published

March 27, 2002

Add a comment...

Supporters

Support the authors with ResearchCoin

Journal

Geophysical Journal International

Topics

DOI

10.1046/j.1365-246x.2002.01556.x

Paper

Paper

Paper

Paper

Uniform postglacial slip-rate along the central 600 km of the Kunlun Fault (Tibet), from 26Al, 10Be, and 14C dating of riser offsets, and climatic origin of the regional morphology

Supporters

Journal

Topics

DOI

Uniform postglacial slip-rate along the central 600 km of the Kunlun Fault (Tibet), from 26Al, 10Be, and 14C dating of riser offsets, and climatic origin of the regional morphology

Supporters

Journal

Topics

DOI