Sources, sinks and long-term cycling of iodine in the hyperarid Atacama continental margin-Reference-Cited by-同舟云学术

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Sources, sinks and long-term cycling of iodine in the hyperarid Atacama continental margin

Published:2015-07 Issue: Volume:161 Page:50-70
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Álvarez Fernanda,Reich Martin,Pérez-Fodich Alida,Snyder Glen,Muramatsu Yasuyuki,Vargas Gabriel,Fehn Udo

Funder

FONDECYT

Centro de Excelencia en Geotermia de los Andes

CONICYT

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference138 articles.

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2. The role of inherited tectono-sedimentary architecture in the development of the central Andean mountain belt: insights from the Cordillera de Domeyko;Amilibia;J. Struct. Geol.,2008

3. Geomorphologic evidence for the late Pliocene onset of hyperaridity in the Atacama Desert;Amundson;Geol. Soc. Am. Bull.,2012

4. The in situ production of radioisotopes in rock matrices with particular reference to the Stripa granite;Andrews;Geochim. Cosmochim. Acta,1989

5. Space-geodetic estimation of the Nazca-South America Euler vector;Angermann;Earth Planet. Sci. Lett.,1999

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