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Siliciclastics

Pematang/Sihapas Siliciclastics Assessment Unit 38080101 ...

ÚÊ ÚÊ Pematang/Sihapas Siliciclastics Assessment Unit 38080101 Central Sumatra Basin Geologic Province 3808 Pematang/Sihapas Siliciclastics

Parameters controlling sonic velocities in a mixed carbonate ...

Parameters controlling sonic velocities in a mixed carbonate- siliciclastics Permian shelf-margin

Back to the Rocks: New Petrophysical Model for Siliciclastics ...

Back to the Rocks: New Petrophysical Model for Siliciclastics Engaging Old Petrological Techniques, #10346 (2011)

Stratigraphic evolution of OligoceneMiocene carbonates and ...

and siliciclastics, East Java basin, Indonesia Essam Sharaf, J. A. (Toni) Simo, Alan R. Carroll, and Martin Shields ABSTRACT The Oligocene–Miocene of East Java is characterized by multiple

Depositional Themes of Mixed Carbonate-siliciclastics in the ...

Depositional Themes of Mixed Carbonate-siliciclastics in the South Florida Neogene: Application to Ancient Deposits

Increased terrigenous influx but no drowning ...

siliciclastics on the Tunisian shelf and in other parts of the tropical arid realm (Weissert, 1990) during the mid-Late Aptian might have been

chrono-model

1 ABSTRACT: Recent drilling of continuous cores in southernmost Florida has documented a thick unit of upper Neogene siliciclastics subjacent to surficial shallow-water Quaternary carbonates exposed on islands of the Florida Keys.

Transgressive-Regressive Cycles: Application to Petroleum ...

Transgressive-Regressive Cycles: Application to Petroleum Exploration for Hydrocarbons Associated with Cretaceous Shelf Carbonates and Coastal and Fluvial-Deltaic Siliciclastics, Northeastern Gulf of Mexico

LAURA A. GUERTIN

ABSTRACT: Recent drilling of continuous cores in southern most Florida has documented a thick unit of upper Neogene siliciclastics subjacent to surfi cial shallow-water Quaternary

DEPOSITIONAL HISTORY OF THE ATOKAN SUCCESSION (LOWER ...

aerially restricted, lower Atokan fluvial to shallow-marine siliciclastics followed by pervasive carbonate deposition. In general, Atokan-age siliciclastics dominated