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Indidura Formation

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Series: SEPM Special Publication, SEPM Special Publication
Published: 01 January 2009
DOI: 10.2110/sepmsp.093.171
EISBN: 9781565762978
... TABLE 2. —Indidura Formation, sample stratigraphic assignment, total organic carbon (TOC), total carbonate, stable isotopes, and elemental concentrations. Average C/T Shale is from Brumsack (2006) ; average shale is from Wedepohl (1971 , 1991 ); Low and High black shale is from Quinby-Hunt...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 1938
GSA Bulletin (1938) 49 (1): 69–150.
Journal Article
Journal: GSA Bulletin
Published: 01 January 1949
GSA Bulletin (1949) 60 (1): 89–176.
... of lower and middle Albian age, the Cuesta del Cura limestone of upper Albian age, the Indidura formation of Cenomanian-Turonian age, and the Parras shale of Coniacian-Santonian age. The La Peña formation contains a large fauna of mollusks, brachiopods, and echinoids. Ammonites dominate the fauna...
Series: Special Publications of the Society of Economic Geologists, Special Publications of the Society of Economic Geologists
Published: 01 January 2001
DOI: 10.5382/SP.08.07
EISBN: 9781629490328
..., Cuesta del Cura, and Indidura Formations. A dacite flow-dome complex of lower Tertiary age unconformably overlies the sediments and a middle Tertiary sequence of rhyolite tuffs overlies the dacites. Four phases of deformation are seen in the district including tight folding and local thrust faulting...
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Series: Memoir - AAPG, Memoir - AAPG
Published: 01 January 2001
DOI: 10.1306/M75768C9
EISBN: 9781629810638
... in the Aptian ( Dickinson and Lawton, 2001 ) or the succeeding continental-margin arc that commenced in the Albian. The presence of thick submarine tuffs of early Late Cretaceous age at the top of the Indidura Formation and in its equivalent, the Caracol Formation, provides a case for the latter...
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Journal Article
Journal: Economic Geology
Published: 01 December 1988
Economic Geology (1988) 83 (8): 1802–1829.
... at the junction between the Sierra Madre Oriental, the Sierra Madre Occidental, and the Mesa Central. Host sediments are the Lower Cretaceous Aurora and Cuesta del Cura limestones and the Upper Cretaceous Indidura and/or Caracol Formations. Mineralization is spatially and temporally associated with a 33-m.y.-old...
Journal Article
Journal: GSA Bulletin
Published: 01 January 1967
GSA Bulletin (1967) 78 (1): 59–76.
... formations (Barril Viejo, Patula, La Mula, Taraises-Cupido, La Peña, Aurora-Cuesta del Cura), which are more than 7000 feet thick, form the major part of the mountain mass. Upper Cretaceous rocks (Indidura) and alluvial debris, together more than 500 feet thick, constitute minor mappable units. Younger...
Journal Article
Published: 01 July 2011
Journal of Paleontology (2011) 85 (4): 719–743.
...Dario G. Lazo; Susana E. Damborenea Abstract The Cretaceous Huitrín Formation in west-central Argentina records the final connection of the Neuquén Basin to the Pacific Ocean. This formation is comprised of a variety of continental to marginal-marine sediments deposited behind an Andean volcanic...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 2018
AAPG Bulletin (2018) 102 (10): 1963–1984.
... Member corresponds to the overlying Austin Chalk ( Maxwell et al., 1967 ; Peschier, 2006 ). In Coahuila and Chihuahua, Mexico, the Eagle Ford Formation is known as the Indidura and Ojinaga Formations ( Whitcomb, 2001 ; Peschier, 2006 ). The boundary between the Buda Limestone and the Eagle Ford...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1961
AAPG Bulletin (1961) 45 (9): 1504–1522.
... and paleontology of the Indidura Formation, Coahuila, Mexico : Geol. Soc. America Bull. , v. 49 , p. 69 – 149 . Kellum , L. B. , Imlay , R. W. , and Kane , W. G. , 1936 , Evolution of the Coahuila Peninsula, Mexico : Part 1, Relation of structure, stratigraphy, and igneous activity...
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Image
Figure 1. Location and geologic map of La Popa basin. Symbols—Jm, Minas Vie...
in > Geology
Published: 01 February 2005
Figure 1. Location and geologic map of La Popa basin. Symbols—Jm, Minas Viejas Formation; Kl, Lower Cretaceous carbonate strata; Ki, Indidura Formation; Kp, Parras Shale; Km, Muerto Formation; Potrerillos Formation: Kpl, Cretaceous part; Kpc, Cuchilla Tongue; Kpd, Delgado Sandstone Member; Tpu
Image
(A) Geologic map of La Popa basin. Cross section line of (B) indicated. Ins...
Published: 01 April 2017
Zuloaga Limestone to Indidura Formation (Fm). From Lawton et al. (2001) . K = Cretaceous; Mbr = Member; Ss = Sandstone.
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1970
AAPG Bulletin (1970) 54 (7): 1245–1270.
... and chert unit between the massive rudistid limestone of the Aurora Formation below and the thin-bedded, clayey limestone of the Indidura Formation above. The term “formation” is preferable to “limestone” because the Cuesta del Cura contains abundant chert stringers and some shale, as well as limestone...
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Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2003
DOI: 10.1306/M79877C16
EISBN: 9781629810546
... the underlying Indidura Formation and overlying Difunta Group are conformable and gradational ( Figure 7 ). The lower boundary is marked by a gradational contact between deep-water gray calcareous mudstone of the Indidura Formation. The Parras Shale coarsens gradually upward into the sandstone-prone Cerro del...
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Image
Cross sections in La Popa basin showing (a) regional structures, including ...
Published: 01 May 2003
flexure on the northeast-dipping fold limb. Short red lines are measured bedding attitudes. Strata include Kac = carbonate lentils equivalent to the Aptian Cupido and Albian Aurora formations; Ki = basinal carbonates of the Cenomanian to Santonian Indidura Formation; Kp = Campanian Parras shale; Km
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1944
AAPG Bulletin (1944) 28 (8): 1077–1195.
..., Coahuila. At the last mentioned locality it has been called the lower member of the Indidura formation and represents both the upper Albian and the lower Cenomanian. At these localities it overlies areas that were landmasses, or marginal to landmasses, in Upper Jurassic time. A third facies of upper...
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Series: Memoir - AAPG, Memoir - AAPG
Published: 01 January 2001
DOI: 10.1306/M75768C10
EISBN: 9781629810638
..., clayey limestone, and sandstones of the Indidura Formation ( Kelly, 1936 ). The Eagle Ford Formation represents a TST deposited in a middle-neritic environment. A late Cenomanian to early Turonian age is indicated by the presence of Inoceramus labiatius, Clavihedbergella simplex , Hedbergella amabilis...
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Series: GSA Special Papers
Published: 01 January 2007
DOI: 10.1130/2007.2422(08)
... of right-lateral slip. At least four reactivation events have been recognized along the San Marcos fault. The first, in Neocomian time, was normal and triggered deposition of the San Marcos Formation. The second reactivation of the San Marcos fault involved reverse slip during Paleogene time, and it must...
Series: GCSSEPM, GCSSEPM
Published: 01 December 2016
DOI: 10.5724/gcs.15.35.0450
EISBN: 978-1-944966-10-2
... basins, where it is also a proven source rock ( Núñez-Useche et al. , 2014 , 2016 ). Elsewhere in northeastern Mexico, the Eagle Ford-equivalent Indidura and Agua Nueva formations contain well-studied paleontological and geochemical records tying low-oxygen sediments to the global OAE ( Scholle...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 2010
AAPG Bulletin (2010) 94 (3): 273–291.
... of the Potrerillos Formation based on biomarker data. Thermal and subsidence modeling of the basin indicate that all of the strata in the basin are mature enough to have generated hydrocarbons. The lower part of the stratigraphic section entered the gas generation window, and much of the Cretaceous section and all...
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