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Book Lithofacies  Depositional Environments  and Sequence Stratigraphy of the Pennsylvanian  Morrowan Atokan  Marble Falls Formation  Central Texas

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.

Book The Lithostratigraphy and Depositional History of the Marble Falls Formation  Pennsylvanian  in the Subsurface Immediately North of the Llano Uplift  Central Texas

Download or read book The Lithostratigraphy and Depositional History of the Marble Falls Formation Pennsylvanian in the Subsurface Immediately North of the Llano Uplift Central Texas written by Charles Michael Brown and published by . This book was released on 1983 with total page 430 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Sedimentology and Stratigraphy of Pennsylvanian and Lower Permian Strata  Upper Amsden Formation and Tensleep Sandstone  in North central Wyoming

Download or read book Sedimentology and Stratigraphy of Pennsylvanian and Lower Permian Strata Upper Amsden Formation and Tensleep Sandstone in North central Wyoming written by Dennis Rolland Kerr and published by . This book was released on 1989 with total page 412 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book The Lithostratigraphy  Carbonate Petrography  and Depositional History of the Marble Falls Formation  Pennsylvanian  in the Subsurface of Brown and Mills Counties  Central Texas

Download or read book The Lithostratigraphy Carbonate Petrography and Depositional History of the Marble Falls Formation Pennsylvanian in the Subsurface of Brown and Mills Counties Central Texas written by Richard Stephen Luker and published by . This book was released on 1985 with total page 386 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Bibliography and Index of Geology

Download or read book Bibliography and Index of Geology written by and published by . This book was released on 1990 with total page 1516 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Petroleum Abstracts

Download or read book Petroleum Abstracts written by and published by . This book was released on 1992 with total page 1716 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Petroleum Abstracts  Literature and Patents

Download or read book Petroleum Abstracts Literature and Patents written by and published by . This book was released on 1985 with total page 1406 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Lithofacies of the Salt Wash Member of the Morrison Formation

Download or read book Lithofacies of the Salt Wash Member of the Morrison Formation written by Thomas E. Mullens and published by . This book was released on 1954 with total page 78 pages. Available in PDF, EPUB and Kindle. Book excerpt:

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

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.

Book STRATIGRAPHY OF THE MARBLE FALLS INTERVAL  PENNSYLVANIAN   JACK AND WISE COUNTIES  TEXAS

Download or read book STRATIGRAPHY OF THE MARBLE FALLS INTERVAL PENNSYLVANIAN JACK AND WISE COUNTIES TEXAS written by and published by . This book was released on 2004 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: Five informal stratigraphic units can be recognized on well logs through the Marble Falls interval in the northern Fort Worth basin. Four of the units--an upper limestone, upper shale, lower limestone, and lower shale--are present in the eastern half of Wise County. These units interfinger to the west in Jack County with a heterolithic unit comprised of siltstones, mudstones and claystones. Facies recognized in core through the heterolithic unit and log curve shapes in the limestones and shales reveal shallowing-upward sequences formed as the basin filled. The basin fill contains authochthonous carbonate sediment produced in shallow epeiric seas and siliciciclastic (and perhaps carbonate) debris eroded off rising positive structures such as the Bend arch, Red River arch, Muenster arch, and the Ouachita thrust belt during the Ouachita orogeny. Revised correlations based on additional well control suggest the Comyn Limestone and the Forestburg limestone are the same lithostratigraphic unit.

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

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

Book Depositional Environments of the Pennsylvanian Bremen Sandstone Member and Associated Strata  Pottsville Formation  North Central Alabama

Download or read book Depositional Environments of the Pennsylvanian Bremen Sandstone Member and Associated Strata Pottsville Formation North Central Alabama written by Joanne Mary Shadroui and published by . This book was released on 1986 with total page 344 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Depositional Facies and Environments of the Lower Mineral Wells Formation  Pennsylvanian Strawn Group  North Central Texas

Download or read book Depositional Facies and Environments of the Lower Mineral Wells Formation Pennsylvanian Strawn Group North Central Texas written by Susan Elizabeth Bradshaw and published by . This book was released on 1996 with total page 162 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Depositional Environments for Strata of Composite Section of Frontier Formation  Madison Range  Southwestern Montana

Download or read book Depositional Environments for Strata of Composite Section of Frontier Formation Madison Range Southwestern Montana written by Russell G. Tysdal and published by . This book was released on 1991 with total page 32 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Depositional Environments and Paleogeography of the Pennsylvanian Upper Amsden Formation and Tensleep Sandstone in the Seminoe Mountains  South central Wyoming

Download or read book Depositional Environments and Paleogeography of the Pennsylvanian Upper Amsden Formation and Tensleep Sandstone in the Seminoe Mountains South central Wyoming written by Philip L. Glover and published by . This book was released on 2000 with total page 216 pages. Available in PDF, EPUB and Kindle. Book excerpt: