The Second-Order Cycle, Carbonate-Platform Growth, and Reservoir, Source, and Trap Prediction

Sarg, J. F.; Markello, James R.; Weber, L.

doi:10.2110/pec.99.11.0011

Cited by 30 publications

(44 citation statements)

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“…Next step, it is common to find thick, high relief, and often backstepping carbonate successions in Wonosari Formation. It was regionally formed during Oligo-Miocene (Sarg et al, 1999;Miller et al, 2005). 2.…”

Section: Discussionmentioning

confidence: 99%

Allostratigraphy of Punung Paleoreef based on Lithofacies Distributions, Jlubang Area, Pacitan Region-East Java

Premonowati¹,

Prastistho²,

Firdaus³

2012

Indonesian J. Geosci.

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Lithologically, Punung Formation as a paleoreef comprises coral boundstone rhodolith, algal grainstone, algal packstone, algal wackestone, algal floatstone, and algal rudstone. It is dominated by red algae and had formed a fringing reef in a warmly shallow marine environment. They built seven phases of paleoreef complex. Each paleoreef complex has been bounded by a local unconformity that is characterized by caliche. The Jaten Formation has becomes the base of the Punung paleoreef which build up by an angular unconformity contact on uppermost part. It consists of tuffaceous wacky sandstone with silicate cement. The formation as the reef base indicates two factors. The external factor because of the decrease of a volcanic activity and the internal one was caused by the depositional environment of the Jaten Formation becoming shallower. The subsurface runoff systems in many caves (like: Jaran cave and others) have the same southward direction to the dipping direction of algal grainstone lithofacies of Punung Formation. The vertical caves are formed by a jointing system. Keywords

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Section: Discussionmentioning

confidence: 99%

Allostratigraphy of Punung Paleoreef based on Lithofacies Distributions, Jlubang Area, Pacitan Region-East Java

Premonowati¹,

Prastistho²,

Firdaus³

2012

Indonesian J. Geosci.

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“…suggests that this unit is a composite third-order sequence (sensu Weber et al, 1995;Sarg et al, 1999). The sequence is bounded by regional unconformities, and internally, its regional facies stacking pattern indicates a widespread transgression followed by a regression ( Figure 6C).…”

Section: Composite Third-order Sequencementioning

confidence: 98%

“…The sequence-stratigraphic terminology in this article follows the hierarchy set forward by Weber et al (1995) and Sarg et al (1999) for deciphering depositional units. The measured sections were correlated onto four regional cross sections (Figure 1) by directly walking sequence boundaries between sections in closely spaced sections, correlating parasequence stacking patterns and unconformities between farther spaced sections (as outlined in Harris et al, 1999), and integrating the available biostratigraphy.…”

Section: Sequence Stratigraphymentioning

confidence: 99%

High-resolution sequence stratigraphy of the Upper Ordovician Montoya Group, southern New Mexico and western Texas: Outcrop analog of an unconventional chert and carbonate reservoir

Pope¹

2014

Bulletin

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The Upper Ordovician Montoya Group crops out in southern New Mexico and westernmost Texas and records predominantly subtidal deposition on a gently dipping carbonate ramp that was subsequently almost entirely dolomitized. The Montoya Group is a third-order composite sequence composed of six regionally correlative, shallowing-upward, third-order depositional sequences (M0-M5). Sequence M0 has sandstone at its base that is overlain by skeletal packstone-grainstone. Sequence M0 occurs only locally and was likely deposited in a topographic low formed during regional development of the unconformity following El Paso Group deposition. Sequence M1, marking the initial widespread transgression over the Ellenburger unconformity, consists of sandstone updip that passes downramp into skeletal packstone. The highstand systems tract (HST) of M1 consists of a prograding skeletal grainstone that was subaerially exposed upramp. Sequence M2, which contains the second-order maximum flooding surface, has abundant subtidal cherty carbonate at its base, which shallows upward into a widespread, prograding coral packstone-grainstone in the HST. Sequence M3 also contains abundant downramp chert that passes upramp into an aggrading crinoidal shoal and farther upramp into peritidal mudstone. Sequence M4 records an extensive basinward shift in facies as peritidal burrowed and cryptalgalaminated mudstone prograded over subtidal

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“…Sedimentation into the basin was mainly controlled by a combination of rapid subsidence rates coupled with sea level fluctuations that were common during the early Permian (Montgomery, 1996;Mazzullo, 1997;Sarg et al, 1999;Golonka and Kiessling, 2002). The shedding of material off of the platform and shelf are interpreted as occurring during highstands and attributed to the general progradation cycle of the shelf (Mazzullo, 1997).…”

Section: Geologic Backgroundmentioning

confidence: 99%

A Diagenetic Study of the Wolfcamp Shale, Midland Basin, West Texas

Wickard¹,

Elmore²,

Heij³

2016

Proceedings of the 4th Unconventional Resources Technology Conference

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The Second-Order Cycle, Carbonate-Platform Growth, and Reservoir, Source, and Trap Prediction

Cited by 30 publications

References 0 publications

Allostratigraphy of Punung Paleoreef based on Lithofacies Distributions, Jlubang Area, Pacitan Region-East Java

Allostratigraphy of Punung Paleoreef based on Lithofacies Distributions, Jlubang Area, Pacitan Region-East Java

High-resolution sequence stratigraphy of the Upper Ordovician Montoya Group, southern New Mexico and western Texas: Outcrop analog of an unconventional chert and carbonate reservoir

A Diagenetic Study of the Wolfcamp Shale, Midland Basin, West Texas

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