Extreme extension across Seram and Ambon, eastern Indonesia: evidence for Banda slab rollback
The island of Seram, which lies in the northern part of the 180°-curved Banda Arc, has previously been interpreted as a fold-and-thrust belt formed during arc-continent collision, which incorporates ophiolites intruded by granites thought to have been produced by anatexis within a metamorphic sole....
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2013-09-01
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| Series: | Solid Earth |
| Online Access: | http://www.solid-earth.net/4/277/2013/se-4-277-2013.pdf |