Sequence Stratigraphy of the South Texas Oligocene: Understanding the Relationship Between Shale Tectonism and Lowstand Deposition R. Treviño, L.F. Brown,

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Presentation transcript:

Sequence Stratigraphy of the South Texas Oligocene: Understanding the Relationship Between Shale Tectonism and Lowstand Deposition R. Treviño, L.F. Brown, R. Loucks, and U. Hammes Bureau of Economic Geology Jackson School of Geosciences The University of Texas at Austin

A New Depositional Model for the Frio / Vicksburg

Overview Location South Texas Growth-Faulted Subbasins Stratigraphy – Structure Interplay Dynamic Model Exploration Potential

Location Map

Seismic Line in Corpus Christi Bay

Schematic representation - successive growth-faulted intraslope subbasins

Organization of sands (after Mitchum and Van Wagoner, 1991)

Related to the interaction of: Origin of Growth-Faulted Subbasins - gravity tectonics, - relative sea-level changes, - and sediment supply.

Wireline-log sequence stratigraphy Basin-floor fans

Wireline-log sequence stratigraphy Slope fans

Wireline-log sequence stratigraphy Lowstand prograding wedge

Wireline-log sequence stratigraphy Lowstand prograding wedge

Organization of sands

Lowstand systems tract Incised-valleys Incised valleys commonly erode at fault intersections Slope upper - lower Pelagic deposition LST Prograding Wedges ~20 to 40 miles Early Lowstand Systems Tract Depositional systems after Galloway et al., 1982

Schematic representation of successive growth- faulted intraslope subbasins

Dynamic Depositional Model

Offshelf Lowstands overload slope Growth-faulted subbasins younger basinward Similar log facies, different subbasins = different time Deep Potential Conclusions

Acknowledgements Western Geco – Seismic Sabco IBC (now Boss Exploration)

STARR PROGRAM State of Texas Advanced Resource Recovery

Organization of sands (after Mitchum, 1991)

Organization: Seismic view Anahuac HST

Schematic representation of successive growth- faulted intraslope subbasins Organization

Regional dip cross section using S 5 logs Paleo control

Isochron map of lowstand prograding wedges Sediment input (incised valleys) axes

Isopach map of lowstand prograding wedges Incised valley feeder systems

Isopach map of lowstand incised-valley fills

Cross section of incised-valley fills (lowstand)

Wireline-log sequence stratigraphy Lowstand incised-valley fill, transgressive, and highstand systems tracts

Wireline-log sequence stratigraphy Lowstand incised- valley fill, transgressive, and highstand systems tracts

Red Fish Bay S 5 -Benchmark Chart

Section of Red Fish Bay S 5 -Benchmark Charts

Regional correlations of sands So, how do you correlate between subbasins?

Regional dip cross section using S 5 logs

Site-Specific Sequence-Stratigraphic Section Benchmark Charts (S 5 Benchmark Charts) Composite logs with Sequence stratigraphy additional data summarize subbasin geology Promote accurate correlations

Stage in development and filling of growth-faulted intraslope subbasins: Stage 1 Shelf edge ~ ft +/-1000 ft

Stage in development and filling of growth-faulted intraslope subbasins: Stage 2 Turbidity flow

Stage in development and filling of growth-faulted intraslope subbasins: Stage 3 Turbidity flow

Stage in development and filling of growth-faulted intraslope subbasins: Stage 4 Turbidity flow Mobilized basinal shales forming incipient shale ridge

Stage in development and filling of growth-faulted intraslope subbasins: Stage 5 Incised valleys Termination of slope fan deposition

Stage in development and filling of growth-faulted intraslope subbasins: Stage 6 ivf

Stage in development and filling of growth-faulted intraslope subbasins: Stage 7

Schematic representation of successive shifting LST depocenters