Provenance and post-depositional low-temperature evolution of the James Ross Basin sedimentary rocks (Antarctic Peninsula) based on fission track analysis

Abstract Zircon and apatite fission track (AFT) thermochronology was applied to the James Ross Basin sedimentary rocks from James Ross and Seymour islands. The probable sources of these sediments were generated in Carboniferous to Early Paleogene times (∼315 to 60 Ma). The total depths of individual...

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Bibliographic Details
Published in:Antarctic Science
Main Authors: Svojtka, Martin, Nývlt, Daniel, Murakami, Masaki, Vávrová, Jitka, Filip, Jiří, Mixa, Petr
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2009
Subjects:
Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
Antarctic
Antarctic Peninsula
Seymour
Seymour Island
Antarc*
Antarctic Science
Online Access:http://dx.doi.org/10.1017/s0954102009990241
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102009990241

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