Susceptibility and radiometry data used for stratigraphic correlations: case study on Upper Triassic beds in Turkey

Mayrhofer, Susanne; Lukeneder, Alexander

doi:10.1144/sp414.10

Cited by 2 publications

(3 citation statements)

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“…† Gamma-ray spectrometry (GRS) measurements are related to the abundance of the three dominant radioactive elements occurring in sedimentary rocks: K, Th and U. For carbonate rocks, K and Th are interpreted as reflecting clastic GRS curves have often been compared with MS patterns, and differences and similarities can provide insight into detrital and/or diagenetic influences (Bábek et al 2010;Koptíková et al 2010a, b, Koptíková 2011Kozłowski & Sobień 2012;Ellwood et al 2013;Grabowski et al 2013;Chadimova et al 2015;Devleeschouwer et al 2015;Mayrhofer & Lukeneder 2015). In Devonian carbonates from the Barrandian area in the Czech Republic (Požáry-3 section), Koptíková et al (2010a) showed that there is a relatively good correlation between MS and GRS (Fig.…”

Section: Comparison With Other Proxiesmentioning

confidence: 99%

“…Importantly, these correlations need to be framed in a well-developed biostratigraphic framework. Correlations can then be established through different techniques: † By visual correlation of MS peaks (Crick et al 1997;Geršl & Hladil 2004;Da Silva & Boulvain 2006;Bábek et al 2010;Boulvain et al 2010;Michel et al 2010;Dechamps et al 2015;Grabowski et al 2015;Mayrhofer & Lukeneder 2015;Whalen et al 2015). † The MS curve can also be included in a sequence stratigraphic framework (Whalen & Day 2008, 2010Da Silva et al 2010).…”

Section: Application Of Ms As a Correlation Toolmentioning

confidence: 99%

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Magnetic susceptibility application: a window onto ancient environments and climatic variations: foreword

Silva

Whalen

Hladil

et al. 2015

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Magnetic susceptibility (MS) is a powerful tool, which is being applied increasingly on sedimentary rocks to constrain stratigraphic correlations, or as a palaeo-environmental or palaeoclimatic tool. The origin of the magnetic minerals responsible for the variations in MS can be linked to various phenomena such as detrital inputs, pedogenesis, bacterial precipitation or diagenesis. Therefore, it is critical to improve our knowledge of the origin of the MS signal in order to apply it for correlations or as a proxy. Here, we present a synthesis of the techniques that can be applied to get a better understanding of the origin of the MS signal, through comparison with other palaeo-environmental proxies, through magnetic measurements or through dissolution and direct observation of the extracted minerals. We also propose an overview of the different techniques applied in order to use MS as a correlation tool, and we show various examples of successful applications of MS as a recorder of change in past sea-level and climate. We also present the main results and activities of the IGCP-580 project 'Application of magnetic susceptibility as a palaeoclimatic proxy on Palaeozoic sedimentary rocks and characterization of the magnetic signal'.

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Section: Comparison With Other Proxiesmentioning

confidence: 99%

Section: Application Of Ms As a Correlation Toolmentioning

confidence: 99%

Magnetic susceptibility application: a window onto ancient environments and climatic variations: foreword

Silva

Whalen

Hladil

et al. 2015

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“…; Lukeneder et al . ; Lukeneder & Lukeneder ; Lukeneder & Mayrhofer ; Mayrhofer & Lukeneder ). During the Carnian, the sediments around Aşağiyaylabel and Yukariyaylabel in the Tarus Mountains were deposited within an intrashelf setting on the western end of the Cimmerian System (Stampfli & Borel ; Lukeneder et al .…”

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Late Triassic (Julian) conodont biostratigraphy of a transition from reefal limestones to deep‐water environments on the Cimmerian terranes (Taurus Mountains, southern Turkey)

Chen

Lukeneder

2017

Papers in Palaeontology

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Sections at As ßa giyaylabel and Yukariyaylabel, Taurus Mountains, southern Turkey, provide a rare opportunity to investigate conodont faunas in detail across a reef to slope transition. Intensive sampling of limestone beds (wackestones to packstones) through approximately 3 m at these locations has led to the recognition of a new lower Carnian (Julian 1/2) conodont fauna within the Kartoz and Kasimlar formations. Members of the subfamilies Paragondolellinae and Pseudofurnishiinae are recognized. The genus Kraussodontus is reported for the first time from the Taurus Mountains. Mosherella postkockeli and Mosherella praebudaensis sp. nov. occur within the lower Carnian Carbonate Member of the Kasimlar Formation from the Taurus Platform Units. The discovery of the new conodont assemblages from As ßa giyaylabel and Yukariyaylabel facilitates a correlation with faunal assemblages worldwide. F I G . 1 . Position of the As ßa giyaylabel (= Kartoz) and Yukariyaylabel (= Karapinar) sections in the Taurus Mountains (Anatolia, southwest Turkey). A, geography; and B, geology of the investigated area. C, outcrops of Upper Triassic sediments around the area of As ßa giyaylabel and Yukariyaylabel within the the Anamas Daǧ carbonate platform. Investigated sections are indicated as ASI and IV and KAI, II

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Susceptibility and radiometry data used for stratigraphic correlations: case study on Upper Triassic beds in Turkey

Cited by 2 publications

References 56 publications

Magnetic susceptibility application: a window onto ancient environments and climatic variations: foreword

Magnetic susceptibility application: a window onto ancient environments and climatic variations: foreword

Late Triassic (Julian) conodont biostratigraphy of a transition from reefal limestones to deep‐water environments on the Cimmerian terranes (Taurus Mountains, southern Turkey)

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