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New insights into the Early Cambrian igneous and sedimentary history of the Southern Oklahoma Aulacogen from basement well penetrations. Robert E. Puckett Jr., Richard E. Hanson, G. Randy Keller, Matthew E. Brueseke, Casey L. Bulen, Amy M. Eschberger, Stanley A. Mertzman

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New insights into the Early Cambrian igneous and sedimentary history of the Southern Oklahoma Aulacogen from basement well penetrations. Robert E. Puckett Jr., Richard E. Hanson, G. Randy Keller , Matthew E. Brueseke, Casey L. Bulen, Amy M. Eschberger, Stanley A. Mertzman. Hanson et al. 2012. - PowerPoint PPT Presentation

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Page 1: Hanson et al. 2012

New insights into the Early Cambrian igneous and sedimentary history of the Southern Oklahoma Aulacogen from basement well penetrations.

Robert E. Puckett Jr., Richard E. Hanson, G. Randy Keller, Matthew E. Brueseke, Casey L. Bulen, Amy M. Eschberger, Stanley A. Mertzman

Page 2: Hanson et al. 2012

Hanson et al. 2012

Page 3: Hanson et al. 2012

From Keller et al. 2011, modified from Casillas 2004

Residual Gravity Anomaly MapIndicates a series of large gravity highs marking the northwestern extent of the Southern

Oklahoma Aulacogen

Page 4: Hanson et al. 2012

SOA Velocity Model – Upper Crust

From Keller 2012

Page 5: Hanson et al. 2012

Modified from Hanson et al. 2012, Aulacogen geometry from Keller 2011

Residual Gravity Map & Cambrian Igneous Rock Outcrops

Page 6: Hanson et al. 2012

Surface Geological Map Modified from Ham et al, 1954, revised by Johnson, 1990

Washita Valley Fault and Overthrust Penetrations Western Arbuckle Mountains

42 km

42 overthrust drilling penetrations Accessible samples from 29 wells 34 km of uncorrelated igneous section

Page 7: Hanson et al. 2012

37 k

m N

on-C

orre

late

d C

ross

Sec

tion

Page 8: Hanson et al. 2012

Outcrop-Based Generalized Cooling Unit DiagramSurface Exposures of the Carlton Rhyolite in the Wichita Mountains

From Puckett et al. 2011

Page 9: Hanson et al. 2012

Rhyolite Cooling Unit Pan American Oil Co. Moore #1-A Sec.20 T1N-R2W

Page 10: Hanson et al. 2012

Rhyolite Photomicrographs

Page 11: Hanson et al. 2012

Rhy

olite

Geo

chem

istry

Dominantly rhyolites and peralkaline rhyolites

Highly fractionated – Depleted Sr, P, Ti - Typical A-type signature

Typical within Plate, A-type, consistant with emplacement in alaucogen type setting

Page 12: Hanson et al. 2012

37 k

m N

on-C

orre

late

d C

ross

Sec

tion

Moderate to thick basalt and intermediate flows overlap in time with rhyolite production.

Page 13: Hanson et al. 2012

Mafic Rock Geochemistry

Samples classified as basalts to andesites Samples classified as subalkaline-alkalineBasalts to andesites-trachyandesites

Samples plot dominantly as tholeitic basalts

Pan Am Newberry Sec. 13-T1N-R3WPan Am Williams Sec. 20-T1N-R2WPan Am Jarman Sec. 19-T1N-R2W

Page 14: Hanson et al. 2012

Maf

ic R

ock

Geo

chem

istry

Pan Am Newberry Sec. 13-T1N-R3WPan Am Williams Sec. 20-T1N-R2WPan Am Jarman Sec. 19-T1N-R2W

Consistent values with rocks sourced from EMI-OIB magma reservoir

Samples compared with Wichita Mtns. mafic rocks indicating thatRoosevelt Gabbros may be intrusive equivalent of Arbuckle samples

Page 15: Hanson et al. 2012

Mafic Rock Geochemistry

Chemostratigraphic DiagramThree flow packages from Pan Am Williams well. Flow packages can be geochemically correlated between closely space wells

Page 16: Hanson et al. 2012

Phreatomagmatic Interval – Magma in Contact With Ground WaterPan American Oil Co. Whyte #1 Sec. 21-T1N-R1W

Page 17: Hanson et al. 2012

Clastic IntervalPan Am Jarman #1Sec. 24-T1N-R3W

395 m

(182 m to eroded top of volcanic section)

Page 18: Hanson et al. 2012

792 m Cumulative Volcaniclastic Interval Intercalated with RhyoliteFrankfort Oil Co. Sparks Ranch #1 Sec. 32-T1S-R1W

Page 19: Hanson et al. 2012

Schematic Igneous Stratigraphy, Wichita Mountains

Hanson et al. 2011Modified from Hogan and Gilbert, 1998

Page 20: Hanson et al. 2012

37 k

m N

on-C

orre

late

d C

ross

Sec

tion

Page 21: Hanson et al. 2012

Representative Wichita Granite Textures from Arbuckle Basement Wells

Page 22: Hanson et al. 2012

The Southern Oklahoma Aulacogen contains a minimum emplaced volume of 250,000 km3.

Igneous activity was strongly bimodal and voluminous.

Felsic magmas were A-type, mafic magmas have an EMI-OIB signature.

Mafic and Felsic volcanism phases overlap.

Eruption products are lava-dominated - Rhyolitic pyroclastic deposits are limited to thin beds between flows - Basalt pyroclastics originate from phreatomagmatic eruptions.

Cratonic-sourced sedimentation into the rift was active during volcanism

In the Spring of 2014 a two-day Field Seminar will be hosted by the Oklahoma Geological Survey on rift-related igneous rocks in the

Arbuckle and Wichita Mountains outcrop areas.

Summary


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