Lithofacies, Sequence Stratigraphy, and Sedimentology of Desert Creek Platform, Slope, and Basin Carbonates, Southern Margin of the Aneth Complex, Middle Pennsylvanian, Paradox Basin, Utah

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ISBN 13 :
Total Pages : 0 pages
Book Rating : 4.:/5 (134 download)

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Book Synopsis Lithofacies, Sequence Stratigraphy, and Sedimentology of Desert Creek Platform, Slope, and Basin Carbonates, Southern Margin of the Aneth Complex, Middle Pennsylvanian, Paradox Basin, Utah by : Christopher M. Perfili

Download or read book Lithofacies, Sequence Stratigraphy, and Sedimentology of Desert Creek Platform, Slope, and Basin Carbonates, Southern Margin of the Aneth Complex, Middle Pennsylvanian, Paradox Basin, Utah written by Christopher M. Perfili and published by . This book was released on 2020 with total page 0 pages. Available in PDF, EPUB and Kindle. Book excerpt: The Aneth Field in the Paradox Basin (SE Utah) has produced nearly 500 MMbbls of oil from phylloid-algal and oolitic carbonate reservoirs of the lower and upper Desert Creek (Paradox Formation, Middle Pennsylvanian) sequences, respectively. The oil resides in a 150 to 200 foot-thick isolated carbonate platform located in a distal ramp setting on the southwest margin of the Paradox Basin. The horseshoe-shaped platform is roughly 12 miles in diameter with an aerial extent of approximately 144 square miles. Evaluation of the platform-to-basin transition on the leeward (southern) margin of the Aneth Platform, the focus of this study, was made possible through Resolute Energy's 2017 donation of well data and core to the Utah Geological Survey Core Research Center. The lower Desert Creek sequence ranges from 50 to 100 feet in thickness and produces from a succession of phylloid-algal, boundstone-capped parasequences in the Aneth Platform. The upper Desert Creek sequence is generally thinner across the platform and is characterized by a succession of oolite-capped parasequences, except on the southern margin of the platform where it ranges from 80 to 115 feet in thickness. The upper Desert Creek "thick" resulted from southward shedding of platform-derived carbonate sediment and lesser amounts of quartz silt and very fine sand off the low-angle southern platform margin slope. A nine-mile-long, north-south-oriented stratigraphic panel constructed from log and core data permits characterization of thickness and facies trends through the upper Desert Creek from platform (north) to slope to distal basin (south) in the Ratherford unit. In the southern margin, five novel facies for the Aneth Field were analyzed, described, and interpreted using a sequence stratigraphic framework, all of which represent deposition on a gravity-influenced platform-edge slope. It is interpreted that the slope facies association was deposited during transgression and highstand and was generally a result of oversteepened slopes as a function of the carbonate factory on the platform being highly productive. Slope and basin facies range from proximal rudstone and floatstone to thin, graded distal turbidites, the latter of which extend at least five miles into the basin. Compaction of the muddy and fine-grained allochthonous sediment followed by pervasive calcite and anhydrite cementation has destroyed any primary porosity in the platform-derived slope-to-basin sediments.

Lithofacies and Sequence Architecture of the Upper Desert Creek Sequence (middle Pennsylvanian, Paradox Formation) in the Greater Aneth Field, Southern Paradox Basin, Utah

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Total Pages : 67 pages
Book Rating : 4.:/5 (14 download)

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Book Synopsis Lithofacies and Sequence Architecture of the Upper Desert Creek Sequence (middle Pennsylvanian, Paradox Formation) in the Greater Aneth Field, Southern Paradox Basin, Utah by : Evan R. Gunnell

Download or read book Lithofacies and Sequence Architecture of the Upper Desert Creek Sequence (middle Pennsylvanian, Paradox Formation) in the Greater Aneth Field, Southern Paradox Basin, Utah written by Evan R. Gunnell and published by . This book was released on 2018 with total page 67 pages. Available in PDF, EPUB and Kindle. Book excerpt: The Greater Aneth Buildup (GAB) is comprised of the 3rd-order middle Pennsylvanian (Desmoinesian) Desert Creek sequence of the Paradox Formation. A hierarchy of 4th- and 5th- order, carbonate-dominated cycles comprise the Upper Desert Creek (UDC) 4th-order sequence. A SE to NW trending transect line, utilizing core and petrophysical data from six oil and gas wells (from SE to NW wells R-19, Q-16, O-16, J-15, K-430, E-313), revealed deposition of seven carbonated facies within four 5th-order parasequences in the UDC. While each of the seven carbonate facies are present across the transect line, the UDC parasequences are dominated by a shallow-water oolite facies. Laterally and vertically, a general facies transition is evident in each of the four parasequences from a dominantly deeper-water succession of facies in the SE, to a more shallow-water, open marine to restricted lagoon, succession of facies to the NW. Parasequence UDC-3 contains the best representation of this facies transition with the SE wells (R-19, Q-16, and O-16) displaying the deeper-water/mixed algal facies grades into the shoaling oolite facies in the NW wells (J-15, K-430, and E-313). Within UDC strata porosity and permeability correlate well to each other, but poorly to facies type. Porosity and permeability are predominantly controlled by diagenesis. Minor appearances of fibrous isopachus rim cements, and more common micritization (both whole grain and envelope) suggest that early-marine diagenesis occurred within the oolite facies. Meteoric diagenesis is demonstrated by abundant calcite spar, and drusy dogtooth cements within oomoldic pores, intraparticle pores, and interparticle pores, in addition to neomorphism of early marine diagenetic fabrics. Spastolithicooids, stylolitization, and grain brecciation are representative of burial diagenesis within these strata. Dolomitization is present in each of the six studied core, but only in minor amounts.

Lithofacies and Sequence Architecture of the Upper Paradox Formation (middle Pennsylvania) in the Subsurface Northern Blanding Subbasin, Paradox Basin, Utah

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ISBN 13 :
Total Pages : 65 pages
Book Rating : 4.:/5 (13 download)

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Book Synopsis Lithofacies and Sequence Architecture of the Upper Paradox Formation (middle Pennsylvania) in the Subsurface Northern Blanding Subbasin, Paradox Basin, Utah by : Geoffrey William Ritter

Download or read book Lithofacies and Sequence Architecture of the Upper Paradox Formation (middle Pennsylvania) in the Subsurface Northern Blanding Subbasin, Paradox Basin, Utah written by Geoffrey William Ritter and published by . This book was released on 2018 with total page 65 pages. Available in PDF, EPUB and Kindle. Book excerpt: THE PARADOX Basin is a northwest-southeast trending intracratonic basin that formed in southwestern Colorado, southeastern Utah and adjacent parts of Arizona and New Mexico during the late Paleozoic Era. During rise of the adjacent Uncompahgre Uplift (Ancestral Rocky Mountains) the rapidly subsiding basin was filled with over 2000 m of Permo-Pennsylvanian sediments. Stacked depositional sequences accumulated in three roughly parallel facies belts: a northeastern clastic belt (adjacent to uplift), a central salt and black shale belt, and a southwestern carbonate belt. Over 400 million barrels of oil have been extracted from upper Paradox (Desert Creek and Ismay) carbonates in the southern Blanding Subbasin (Greater Aneth Field) since 1956. The sedimentology and sequence stratigraphy of Paradox Shelf strata on the walls of the San Juan River gorge and in the subsurface Aneth Buildup are well documented. Less well documented are the stratigraphy and facies architecture of basinward extensions of upper Paradox sequences in the northern part of the Blanding Subbasin.

Carbonate Sequence Stratigraphy

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Publisher : AAPG
ISBN 13 : 0891813365
Total Pages : 513 pages
Book Rating : 4.8/5 (918 download)

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Book Synopsis Carbonate Sequence Stratigraphy by : Robert G. Loucks

Download or read book Carbonate Sequence Stratigraphy written by Robert G. Loucks and published by AAPG. This book was released on 1983-04-15 with total page 513 pages. Available in PDF, EPUB and Kindle. Book excerpt: Hardcover plus Foldouts

Lithofacies and Sequence Architecture of the Lower Desert Creek Sequence, Middle Pennsylvanian, Aneth, Utah

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ISBN 13 :
Total Pages : 72 pages
Book Rating : 4.:/5 (11 download)

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Book Synopsis Lithofacies and Sequence Architecture of the Lower Desert Creek Sequence, Middle Pennsylvanian, Aneth, Utah by : Chanse James Rinderknecht

Download or read book Lithofacies and Sequence Architecture of the Lower Desert Creek Sequence, Middle Pennsylvanian, Aneth, Utah written by Chanse James Rinderknecht and published by . This book was released on 2017 with total page 72 pages. Available in PDF, EPUB and Kindle. Book excerpt: Middle Pennsylvanian (Desmoinesian) strata of the Lower Desert Creek (LDC) sequence within the sub-surface Greater Aneth Field (GAF) reflect a hierarchy of 4th and 5th order carbonate-dominated cycles. The Lower Desert Creek sequence, along the studied transect are composed of eight carbonate facies depositedon an east-facing shelf. There is a lateral transition from open marine algal buildup from the southeast (cores R-19, Q-16, O-16, and J-15) to a more restricted lagoonal environment to the northwest (core K-430 and E-313).

Facies and Sequence Stratigraphic Evolution of the Mixed Carbonate-siliciclastic Strata, Lower Desmoinesian, Southwest Paradox Basin, Utah

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ISBN 13 :
Total Pages : 710 pages
Book Rating : 4.:/5 (89 download)

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Book Synopsis Facies and Sequence Stratigraphic Evolution of the Mixed Carbonate-siliciclastic Strata, Lower Desmoinesian, Southwest Paradox Basin, Utah by : Gary Lee Gianniny

Download or read book Facies and Sequence Stratigraphic Evolution of the Mixed Carbonate-siliciclastic Strata, Lower Desmoinesian, Southwest Paradox Basin, Utah written by Gary Lee Gianniny and published by . This book was released on 1995 with total page 710 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Upper Pennsylvanian and Lower Permian Shelf-To-Basin Facies Architecture and Trends, Eastern Shelf of the Southern Midland B

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ISBN 13 : 9781970007107
Total Pages : 68 pages
Book Rating : 4.0/5 (71 download)

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Book Synopsis Upper Pennsylvanian and Lower Permian Shelf-To-Basin Facies Architecture and Trends, Eastern Shelf of the Southern Midland B by : Tucker F. Hentz

Download or read book Upper Pennsylvanian and Lower Permian Shelf-To-Basin Facies Architecture and Trends, Eastern Shelf of the Southern Midland B written by Tucker F. Hentz and published by . This book was released on 2017-06 with total page 68 pages. Available in PDF, EPUB and Kindle. Book excerpt: Our study documents the shelf, shelf-edge, slope, and basin-floor depositional facies characteristics, stratigraphic variations, and sedimentation trends of the Missourian Canyon Group and Virgilian-Wolfcampian Cisco Group across the southern Eastern Shelf and the adjacent Midland Basin. The Canyon Group (base Palo Pinto Limestone to top Home Creek Limestone) consists of an aggradational carbonate bank succession having locally prominent reef facies. Similar reef facies continued to accumulate during early Cisco sedimentation. The bank/reef interval, largely equivalent in age to the Horseshoe Atoll complex, is as much as 1,540 ft (469 m) thick in northeastern Coke County and forms an irregular, but distinct, shelf margin throughout the eastern part of the study area. Reef buildups are generally aligned at the margin but also occur as local pinnacles in the platform interior. Canyon basin-floor facies are equivalent to the lower part of the Cline shale ("Wolfcamp D") and consist primarily of dark, organic-rich (>2 percent organics) mudrocks. The overlying Cisco section comprises a series of 13 mudrock, limestone, and sandstone cycles (top Home Creek Limestone to top Coleman Junction Limestone), correlated from outcrop, that collectively form a progradational succession extending from the eastern edge (Bunger Limestone) to the central part of the study area (Coleman Junction Limestone). The top of the Home Creek Limestone coincides with a regional downlap surface for the progradational Virgilian lower Cisco shelf strata. Progressive upward decrease in height of shelf-margin clinoforms indicates that accommodation had markedly decreased during deposition of the upper Cisco Group. The Pennsylvanian-Permian (Virgilian-Wolfcampian) boundary is at the top of the Cline shale in the basin and slope provinces and just above the Crystal Falls Limestone in the shelf area. The thickness of the Wolfcampian section is regionally consistent at the shelf (~700 to 850 ft [~213 to 259 m]), expands markedly basinward to as much as 3,500 ft (1,067 m) into a regional depocenter of high accommodation and high sediment influx associated with slope sedimentation, and then thins into the basin proper (to

Sedimentology and Sequence Stratigraphy of Reefs and Carbonate Platforms

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ISBN 13 : 9780608202990
Total Pages : 75 pages
Book Rating : 4.2/5 (29 download)

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Book Synopsis Sedimentology and Sequence Stratigraphy of Reefs and Carbonate Platforms by : Wolfgang Schlager

Download or read book Sedimentology and Sequence Stratigraphy of Reefs and Carbonate Platforms written by Wolfgang Schlager and published by . This book was released on with total page 75 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Carbonate Sequence Stratigraphy

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ISBN 13 :
Total Pages : pages
Book Rating : 4.:/5 (944 download)

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Book Synopsis Carbonate Sequence Stratigraphy by :

Download or read book Carbonate Sequence Stratigraphy written by and published by . This book was released on 1993 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt:

Lower permian sequence stratigraphy of the western Delaware Basin margin, Sierra Diablo, West Texas

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ISBN 13 :
Total Pages : 528 pages
Book Rating : 4.:/5 (47 download)

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Book Synopsis Lower permian sequence stratigraphy of the western Delaware Basin margin, Sierra Diablo, West Texas by : William M. Fitchen

Download or read book Lower permian sequence stratigraphy of the western Delaware Basin margin, Sierra Diablo, West Texas written by William M. Fitchen and published by . This book was released on 1997 with total page 528 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Lithofacies, Depositional Environments, and Sequence Stratigraphy of the Pennsylvanian (Morrowan-Atokan) Marble Falls Formation, Central Texas

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ISBN 13 :
Total Pages : 518 pages
Book Rating : 4.:/5 (865 download)

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Book Synopsis Lithofacies, Depositional Environments, and Sequence Stratigraphy of the Pennsylvanian (Morrowan-Atokan) Marble Falls Formation, Central Texas by : Stephanie Grace Wood

Download or read book Lithofacies, Depositional Environments, and Sequence Stratigraphy of the Pennsylvanian (Morrowan-Atokan) Marble Falls Formation, Central Texas written by Stephanie Grace Wood and published by . This book was released on 2013 with total page 518 pages. Available in PDF, EPUB and Kindle. Book excerpt: The Pennsylvanian Marble Falls Formation in the Llano Uplift region of the southern Fort Worth Basin (Central Texas) is a Morrowan-Atokan mixed carbonate-siliciclastic unit whose deposition was influenced by icehouse glacioeustatic sea-level fluctuations and foreland basin tectonics. Previous interpretations of the Marble Falls Formation focused on outcrop data at the fringes of the Llano Uplift. This study uses a series of 21 cores to create a facies architectural model, depositional environmental interpretation, and regional sequence stratigraphic framework. On the basis of core data, the study area is interpreted to have been deposited in a ramp setting with a shallower water upper ramp area to the south and a deeper water basin setting to the north. Analysis of cores and thin sections identified 14 inner ramp to basin facies. Dominant facies are: (1) burrowed sponge spicule packstone, (2) algal grain-dominated packstone to grainstone, (3) skeletal foraminiferal wackestone, and (4) argillaceous mudstone to clay shale. Facies stacking patterns were correlated and combined with chemostratigraphic data to improve interpretations of the unit's depositional history and form an integrated regional model. The Marble Falls section was deposited during Pennsylvanian icehouse times in a part of the Fort Worth Basin with active horst and graben structures developing in response to the Ouachita Orogeny. The resulting depositional cycles reflect high-frequency sea-level fluctuations and are divided into 3 sequences. Sequence 1 represents aggradational ramp deposition truncated by a major glacioeustatic sea-level fall near the Morrowan-Atokan boundary (SB1). This fall shifted accommodation basinward and previously distal areas were sites of carbonate HST in Sequence 2 deposition following a short TST phase. Sequence 3 represents the final phase of carbonate accumulation that was diachronously drowned by Smithwick siliciclastics enhanced by horst and graben faulting. These findings contribute to our understanding of the depositional response to glacioeustatic sea-level changes during the Pennsylvanian and can also form the basis for constructing a sedimentological and facies analog for Morrowan to Atokan shallow- to deepwater carbonates in the Permian Basin and the northern Fort Worth Basin.

Sequence Stratigraphy of Foreland Basin Deposits

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Publisher : Aapg
ISBN 13 : 9780891813439
Total Pages : 0 pages
Book Rating : 4.8/5 (134 download)

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Book Synopsis Sequence Stratigraphy of Foreland Basin Deposits by : J. C. Van Wagoner

Download or read book Sequence Stratigraphy of Foreland Basin Deposits written by J. C. Van Wagoner and published by Aapg. This book was released on 1995 with total page 0 pages. Available in PDF, EPUB and Kindle. Book excerpt: This memoir, which grew out of an Exxon-led, AAPG-sponsored field trip, discusses concepts and applications of sequence stratigraphy. Following a description and historical perspective of the terminology used, 14 papers discuss topics such as models for topset play types; the sequence stratigraphic significance of trace fossils; lateral variability in the Campanian and lower Maastrichtian of the western interior seaway; facies architecture of parasequences; controls on sequence stacking; stratigraphy of Turonian-Santonian strata; sequence, parasequence, and intraparasequence architecture of the grassy member; and high-frequency sequence stratigraphy and paleogeography of the Kenilworth member. The papers are accompanied by excellent fold-out photos and diagrams--in bandw and color. Annotation copyright by Book News, Inc., Portland, OR

Sedimentary Response to Intrabasinal Salt Tectonism in the Upper Triassic Chinle Formation, Paradox Basin, Utah

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ISBN 13 :
Total Pages : 44 pages
Book Rating : 4.3/5 (91 download)

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Book Synopsis Sedimentary Response to Intrabasinal Salt Tectonism in the Upper Triassic Chinle Formation, Paradox Basin, Utah by : Joseph E. Hazel

Download or read book Sedimentary Response to Intrabasinal Salt Tectonism in the Upper Triassic Chinle Formation, Paradox Basin, Utah written by Joseph E. Hazel and published by . This book was released on 1994 with total page 44 pages. Available in PDF, EPUB and Kindle. Book excerpt: A multidisciplinary approach to research studies of sedimentary rocks and their constituents and the evolution of sedimentary basins, both ancient and modern.

Carbonate Sedimentology and Sequence Stratigraphy

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ISBN 13 : 9789990118056
Total Pages : pages
Book Rating : 4.1/5 (18 download)

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Book Synopsis Carbonate Sedimentology and Sequence Stratigraphy by :

Download or read book Carbonate Sedimentology and Sequence Stratigraphy written by and published by . This book was released on 2006 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt:

Sedimentation and Stratigraphy of Carbonate Rock Sequences

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ISBN 13 :
Total Pages : 296 pages
Book Rating : 4.:/5 (318 download)

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Book Synopsis Sedimentation and Stratigraphy of Carbonate Rock Sequences by : American Geophysical Union

Download or read book Sedimentation and Stratigraphy of Carbonate Rock Sequences written by American Geophysical Union and published by . This book was released on 1989 with total page 296 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Late Quaternary Stratigraphic Evolution of the Northern Gulf of Mexico Margin

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Publisher : SEPM Soc for Sed Geology
ISBN 13 :
Total Pages : 328 pages
Book Rating : 4.:/5 (318 download)

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Book Synopsis Late Quaternary Stratigraphic Evolution of the Northern Gulf of Mexico Margin by : John B. Anderson

Download or read book Late Quaternary Stratigraphic Evolution of the Northern Gulf of Mexico Margin written by John B. Anderson and published by SEPM Soc for Sed Geology. This book was released on 2004 with total page 328 pages. Available in PDF, EPUB and Kindle. Book excerpt: Late Quaternary stratigraphic evolution of the north Gulf of Mexico margin : a synthesis -- High-resolution stratigraphy of a sandy, ramp-type margin, Apalachicola, Florida -- Late Quaternary stratigraphic evolution of the Alabama-west Florida outher continental shelf -- late Quaternary geology of the northeastern Gulf of Mexico shelf : sedimentology, depositional history, and ancient analogs of a major shelf sand sheet of teh modern transgressive systems tract -- Sequence stratigraphy of a continental margin subjected to low-energy and low-sediment-supply environmental boundary conditions : late Pleistocene-Holocene deposition offshore Alabama -- Late Quaternary deposition and paleobathymetry at the shelf-slope transition, ancestral Mobile River delta complex, northeastern Gulf of Mexico -- Depositional architecture of the Lagniappe Delta : sediment characteristics, timing of depositional events, and temporal relations with adjacent shelf-edge deltas -- Foraminiferal biostratigraphy and paleoenvironments of the Pleistocene Lagniappe Delta and related section, northeastern Gulf of Mexico -- Late Quaternary stratigraphic evolution of the west Lousiana-east Texas continental shelf -- Late Quaternary Brazos and Colorado deltas, offshore Texas, their evolution and the factors that controlled their deposition -- Late Quaternary evolution of the wave-storm-dominated Central Texas Shelf -- Late Quaternary evolution of the Rio Grande Delta.

The Sequence Stratigraphy of Fine-grained Sediments and Transform Margin Basins

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ISBN 13 :
Total Pages : 278 pages
Book Rating : 4.:/5 (14 download)

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Book Synopsis The Sequence Stratigraphy of Fine-grained Sediments and Transform Margin Basins by : Bryce William Hoppie

Download or read book The Sequence Stratigraphy of Fine-grained Sediments and Transform Margin Basins written by Bryce William Hoppie and published by . This book was released on 1996 with total page 278 pages. Available in PDF, EPUB and Kindle. Book excerpt: