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Unusual Intraclastic Limestones In Lower Triassic

Unusual Intraclastic Limestones In Lower Triassic

Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the endPermian mass extinction January 2002 Sedimentology 462303 - 316

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  • Unusual Intraclastic Limestones In Lower Triassic

    Unusual Intraclastic Limestones In Lower Triassic

    Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the endPermian mass extinction January 2002 Sedimentology 462303 - 316

  • Unusual Intraclastic Limestones In Lower Triassic

    Unusual Intraclastic Limestones In Lower Triassic

    Read Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the endPermian mass extinction Sedimentology on DeepDyve the largest online rental service for scholarly research with thousands of academic publications available at your fingertips

  • Pdf Unusual Intraclastic Limestones In Lower Triassic

    Pdf Unusual Intraclastic Limestones In Lower Triassic

    Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the end-Permian mass extinction

  • Unusual Intraclastic Limestones In Lower Triassic

    Unusual Intraclastic Limestones In Lower Triassic

    Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the end-Permian mass extinction Wignall Paul B. Twitchett Richard J

  • Anachronistic And Unusual Carbonate Facies In

    Anachronistic And Unusual Carbonate Facies In

    Wignall PB Twitchett RJ 1999 Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the end-Permian mass extinction

  • Giant Induan Oolite A Case Study From The Lower

    Giant Induan Oolite A Case Study From The Lower

    Particular unusual giant oolites within a set of oolitic-bank limestones with thicknesses of more than 40 m in the top part of the Lower Triassic Induan Daye Ruiping Formation at the Lichuan section in the western part of Hubei Province in South China represent an important sedimentological phenomenon in both the specific geological period

  • Giant Induan Oolite A Case Study From The Lower

    Giant Induan Oolite A Case Study From The Lower

    Particular unusual giant oolites within a set of oolitic-bank limestones with thicknesses of more than 40 m in the top part of the Lower Triassic Induan Daye Ruiping Formation at the Lichuan

  • Chapter 12 Environmental Trends Of Early Triassic

    Chapter 12 Environmental Trends Of Early Triassic

    The Permo-Triassic transition in Spitsbergen 3Cot chemostratig- raphy Fe and S geochemistry facies fauna and trace fossils. Geol. Mag. 1351 47-62. Wignall P.B. Twitchett R.J. 1999. Unusual intraclastic limestones in Lower Triassic carbonates and their bear- ing on the aftermath of the end-Permian mass extinction

  • Grains Nonskeletal Grains Intraclasts And

    Grains Nonskeletal Grains Intraclasts And

    Intraclast - A fragment of penecontemporaneous commonly weakly consolidated carbonate sediment that has been eroded and redeposited generally nearby within the same depositional sequence in which it formed Folk 1959 and 1962.. Lumps - In modern sediments irregular composite aggregates of silt- or sand-sied carbonate particles that are cemented together at points of contact in ancient

  • Protointraclasts Texture Of Some Werfenian

    Protointraclasts Texture Of Some Werfenian

    SUMMARY Petrographic examination of some Werfenian limestones of the Dolomite region in northeastern Italy has revealed these iimestones to show an unusual granular texture. This texture seems to have originated during an early resedimentation attempt when the sediments in which they occur were still water impregnated. Because these pseudograins never existed as free clastic entities

  • Diversity And Distribution Of Triassic   Cambridge Core

    Diversity And Distribution Of Triassic Cambridge Core

    Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the end-Permian mass extinction. Sedimentology 46 303 316 . Wignall P. B. and Twitchett R. J. 2002

  • Subtidal Flatpebble Conglomerate From

    Subtidal Flatpebble Conglomerate From

    Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the end-Permian mass extinction. Sedimentology Vol. 46 Issue. 2 p. 303. agree to abide by our usage policies. If this is the first time you use this feature you will be asked to authorise Cambridge Core to connect with your service

  • Microfacies Data Matrix And Grains  Springerlink

    Microfacies Data Matrix And Grains Springerlink

    Wignall P.B. Twichett R.J. 1999 Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermaths of the end-Permian mass extinction. Sedimentology 46 303316 CrossRef Google Scholar

  • Multiproxy Palaeoclimate Reconstruction Of The

    Multiproxy Palaeoclimate Reconstruction Of The

    1999. Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the end-Permian mass extinction. 320 2007. Updated world map of the KoppenGeiger climate classification. 2005

  • New Triassic Literature  Michigan State University

    New Triassic Literature Michigan State University

    Response of Triassic reef coral communities to sea-level fluctuations storms and sedimentation Evidence from a spectacular outcrop Adnet Austria. Facies 40 229-279. Bertling M. 1999. Taphonomy of trace fossils at omission surfaces Middle Triassic East Germany. Palaeogeogr

  • Source And Depositional Processes Of Coarsegrained

    Source And Depositional Processes Of Coarsegrained

    Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the end-Permian mass extinction. Sedimentology 46 303-316. Ziegler W. Sandberg A. S. 1990

  • Sedimentology Of Reefal Buildups Of The Xianndong

    Sedimentology Of Reefal Buildups Of The Xianndong

    The reefs in the Xianndong Formation Cambrian Series 2 are the oldest archaeocyathanmicrobial bioconstructions in China but the details of their microbial structures have not been previously described. However a new section at Tangjiahe site northern Sichuan Province contains very well-preserved microbial fabrics that provide these details and is described in this study

  • Acta Geologica Polonica  Home Icm

    Acta Geologica Polonica Home Icm

    Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the end-Permian mass extinction. Sedimentology 46 303316. 94

  • Controls On The Formation Of Microbially Induced

    Controls On The Formation Of Microbially Induced

    The lack of storm facies is likely to record an unusual Early Triassic climatic regime. It is notable that the Lower Triassic strata of Spitsbergen were deposited at a similar latitude 45N on an ocean-facing shelf and record only minor rare storm events Wignall et al. 2016

  • Early Triassic Griesbachian Microbial Mounds In The

    Early Triassic Griesbachian Microbial Mounds In The

    Wignall PB Twitchett RJ. Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the end-Permian mass extinction. Sedimentology. 1999462303316. View Article Google Scholar 25. Groves JR Altiner D Boyce M Craig BJ

  • Geologic Note Authors  Stanford Earth

    Geologic Note Authors Stanford Earth

    2014-3-23GEOLOGIC NOTE Lower Triassic oolites of the Nanpanjiang Basin This article focuses on the oolitic limestones and dolostones within the Lower Triassic ramp- Lower Triassic strata contain numerous unusual facies and diagenetic features that have been Figure 14. Petrographic characteristics of platform-margin oolite grainstone facies

  • Diagenesis And Geochemistry Of Upper Muschelkalk

    Diagenesis And Geochemistry Of Upper Muschelkalk

    2012-1-31Diagenesis and Geochemistry of Upper Muschelkalk Triassic Buildups and Associated Facies in Catalonia NE Spain a paper dedicated to Francesc Calvet Carbonate buildups are well developed in the Triassic Upper Muschelkalk of eastern Spain in the La Riba Unit but they are completely dolomitised

  • Songetal2012epsl

    Songetal2012epsl

    2013-6-1Unusual intraclastic limestones in Lower Triassic carbonates and their bearing on the aftermath of the end-Permian mass extinction. Sedimentology 46

  • Microbial Deposits In The Aftermath   Wiley Online

    Microbial Deposits In The Aftermath Wiley Online

    In association with microbialites LO and LON are dominated by ooids. Ooids are not rare or unusual components of Phanerooic carbonates they are widespread in Lower Triassic platforms and are often associated with microbialites or synsedimentary sea floor cements Lehrmann et al. 2012 Woods 2013. The LM is observed in low tideenergy