Page 314 - Carbonate Platforms Facies, Sequences, and Evolution

© 1990 The International Association of Sedimentologists ISBN: 978-0-632-02758-3 James Lee Wilson, Paul D. Crevello, J. Rick Sarg, J. Fred Read 291 * Research conducted at Earth Science Board, University of California, Santa Cruz 95064, USA. duction zone. oceanic nappe emplacement as the Oman continental margin approached a northward-dipping sub­ steepening and deepening of the slope, accompanied by faulting on the Arabian platform, preceded Later, a carbonate ramp was able to prograde over the drowned platform. In la

basin.

Carbonate Platforms: Facies, Sequences and Evolution Edited by Maurice E. Tucker,

Tectonism along
F.

and Geo physics,
Sediments. (1990) 9, 291-323
the platform
WATTS*
With tectonic quiescence this basin
and
C.
MS 919 Denver,
margin, supply
D.
Geo physical Institute,
of

platform
BLOME
of a Cretaceous ocean basin,
Colorado 80225,
USA
Oman

carbonate sediment,
CCD) or greater supply of carbonate
and
developed ramp-like margins along which mass
formed along the passive continental margin slope
the extensive shallow-marine Arabian carbonate platform and the deep-oceanic Hawasina
Siliceous sedimentation resulted from tectonically-induced deepening of the ocean basin,
and syn-orogenic sediments of
University of Alaska, Fairbanks 99775,