Non-steady long-term uplift rates and Pleistocene marine terrace development along the Andean margin of Chile (31°S) inferred from 10Be dating-Reference-Cited by-同舟云学术

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Non-steady long-term uplift rates and Pleistocene marine terrace development along the Andean margin of Chile (31°S) inferred from 10Be dating

Published:2009-01 Issue:1-2 Volume:277 Page:50-63
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Saillard M.,Hall S.R.,Audin L.,Farber D.L.,Hérail G.,Martinod J.,Regard V.,Finkel R.C.,Bondoux F.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference78 articles.

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2. Bending the Bolivian orocline in real time;Allmendinger;Geology,2005

3. Middle Miocene climatic change in the Atacama Desert, Northern Chile — evidence from supergene mineralization at La Escondida;Alpers;Geological Society of America Bulletin,1988

4. Origin, structure and exposure history of a wave-cut platform more than 1 Ma in age at the coast of northern Spain: a multiple cosmogenic nuclide approach;Alvarez-Marrón;Geomorphology,2008

5. The generation and degradation of marine terraces;Anderson;Basin Research,1999

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4. Uplift rate calculation based on the comparison between marine terrace data and river profile analysis: A morphotectonic insight from the Ionian coastal belt of Basilicata, Italy;Geomorphology;2024-02

5. Variability of quaternary marine terraces and uplift rates in the Andean coastal zone at 23°S;Quaternary Science Reviews;2024-01

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