Is spreading prolonged, episodic or incipient in the Andaman Sea? Evidence from deepwater sedimentation
© 2014 Elsevier Ltd. The Central Andaman Basin (CAB) is generally accepted to be a site of continuous sea floor spreading since the Early Pliocene (~4.0. Ma). The adjacent Alcock and Sewell Rises, and part of the East Andaman basin have been interpreted as probable Miocene oceanic crust. Published s...
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| Main Authors: | , |
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| Format: | Journal |
| Published: |
2018
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| Subjects: | |
| Online Access: | https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=84920737447&origin=inward http://cmuir.cmu.ac.th/jspui/handle/6653943832/44396 |
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| Institution: | Chiang Mai University |
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