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| Titel |
Fission Track Analysis on Junggar Basin peripheral orogen and Its Geological Significance |
| VerfasserIn |
Wei Li, JianMin Hu, Hongjie Qu |
| Konferenz |
EGU General Assembly 2010
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| Medientyp |
Artikel
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| Sprache |
Englisch
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| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 12 (2010) |
| Datensatznummer |
250042252
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| Zusammenfassung |
| Central Asian Orogenic Belt is the world’s Phanerozoic crustal growth and transformation of
the most significant areas. It is a giant suture zone formed by Paleo-Asian Ocean subduction
which located in between the Siberian Plate and Sino-Korean, Tarim Plate.Northern Xinjiang
is located in the southern section of Central Asian Orogenic Belt. Today It presents a basin
and range landscape. Junggar Basin is located between the Altai Mountain and
Tianshan(Figure 1). Paleozoic tectonic evolution of northern Xinjiang to become a hot
research topic, however, following the closure of the Paleo-Asian Ocean tectonic evolution of
intracontinental, in particular Uplift history of the margin of the Junggar Basin is not clear.
This paper attempts by the margin of the Junggar Basin, Late Paleozoic magmatic rocks of
the apatite, zircon fission-track studies, to reveal the law of uplift of margin of the Junggar
Basin since the Mesozoic.
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