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Geomorphological evidence of carbonate build-up demise on equatorial margins: A case study from offshore northwest Australia
2019
Marine and Petroleum Geology
The demise of Miocene carbonate build-ups in the Browse Basin, Northwest Australia, has been explained as relating to geological and oceanographic processes. These include accelerated tectonic subsidence driven by subduction, ocean cooling following the mid-Miocene climate optimum, nutrient excess, poisoning by sediment drifts and local erosion driven by current winnowing, occurring discretely or simultaneously. Here, we critically assess the evidence for these different mechanisms using a
doi:10.1016/j.marpetgeo.2019.03.006
fatcat:jf3ukbvu5fh7badjujpc6ibku4