1887

Abstract

The Baram Delta province of Brunei (northwest Borneo) is a Tertiary delta system built up upon an active margin. Hence, the structures observed in Brunei are the result of a complex interaction between gravity-driven deltaic tectonics and transpressive tectonics associated with the active margin.

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/content/papers/10.3997/2214-4609.201405827
2003-09-08
2020-10-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405827
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