Conesa, Gilles A. R. et al. (2006): Biosedimentary and paleoenvironmental evolution of the southern Marion Platform from the middle to late Miocene (northeast Australia, ODP Leg 194, Sites 1196 and 1199)

Leg/Site/Hole:
ODP 194
ODP 194 1196
ODP 194 1199
Identifier:
2006-075596
georefid

10.2973/odp.proc.sr.194.005.2005
doi

Creator:
Conesa, Gilles A. R.
Universite d'Aix-Marseille I, Centre de Sedimentologie-Paleontologie, Marseille, France
author

Favre, Eric
National Science Foundation, United States
author

Muench, Phillipe
Ocean Drilling Program, United States
author

Dalmasso, Helene
Christian-Albrechts-Universitaet zu Kiel, Federal Republic of Germany
author

Chaix, Christian
University of Hawaii at Manoa, United States
author

Identification:
Biosedimentary and paleoenvironmental evolution of the southern Marion Platform from the middle to late Miocene (northeast Australia, ODP Leg 194, Sites 1196 and 1199)
2006
In: Anselmetti, Flavio S., Isern, Alexandra R., Blum, Peter, Andresen, Nils, Birke, Tesfaye Kidane, Bracco Gartner, Guido L., Burns, Stephen J., Conesa, Gilles A. R., Delius, Heike, Dugan, Brandon, Eberli, Gregor P., Ehrenberg, Stephen N., Fuller, Michael D., Muller, Pamela Hallock, Hine, Albert C., Howell, Michael W., John, Cedric M., Karner, Garry D., Kindler, Pascal F., Olson, Brooke E., Sasaki, Keiichi, Stewart, Duncan, Wei, Wuchang, White, Timothy S., Wood, Jason L., Yamada, Tsutomu, Proceedings of the Ocean Drilling Program; constraining Miocene sea level change from carbonate platform evolution, Marion Plateau, northeast Australia; covering Leg 194 of the cruises of the drilling vessel JOIDES Resolution; Townsville, Australia, to Apra Harbor, Guam; Sites 1192-1199; 3 January-2 March 2001
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
194
The Southern Marion Plateau (SMP) represents a vertical stacking of Miocene carbonate platform deposits. Two sites (1196 and 1199) were drilled on top of this plateau, penetrating a 663-m carbonate succession of bioclastic and reefal sedimentary bodies. The study focuses on the least dolomitized 410-m-thick upper part of the succession, which is middle to late Miocene in age. Sedimentological and paleontological studies were conducted at both sites in order to propose a paleoenvironmental model and its evolution through the Miocene age. Six main microfacies of possible environmental significance were defined using statistical multivariate analyses, based on the recognition and point counting of 24 biogenic components. Depositional environment reconstructions are proposed as well as the biosedimentary and the environmental evolution regarding seismic architectures, stratigraphy, biosedimentology, and microfacies analysis. The SMP platform mainly results from a vertical stacking of lens-shaped bodies in homoclinal to distally steepened ramp settings.
English
Coverage:Geographic coordinates:
North:-20.5800
West:152.5100East: 152.5500
South:-21.0100

Stratigraphy; bioclastic sedimentation; biostratigraphy; Cenozoic; Coral Sea; cores; depositional environment; geophysical methods; geophysical profiles; geophysical surveys; Leg 194; lithostratigraphy; marine environment; marine sediments; Marion Plateau; microfacies; middle Miocene; Miocene; Neogene; Ocean Drilling Program; ODP Site 1196; ODP Site 1199; Pacific Ocean; paleo-oceanography; paleoenvironment; reef environment; sedimentation; sediments; seismic methods; seismic profiles; South Pacific; Southwest Pacific; surveys; Tertiary; upper Miocene; West Pacific;

.