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Magnetic susceptibility application : a window onto ancient environments and climatic variations / edited by A.C. Da Silva, University of Liège, Belgium, M.T. Whalen, University of Alaska Fairbanks, USA, J. Hladil, AS CR, v.v.i. (Academy of Sciences), Czech republic, L. Chadimova, AS CR, v.v.i. (Academy of Sciences), Czech republic, D. Chen, Chinese Academy of Sciences, China, S. Spassov, Geophysical Centre of Dourbes, Belgium, F. Boulvain, University of Liège, Belgium, and X. Devleeschouwer, Université Libre de Bruxelles, Belgium.
LIBRA QC754.2.S8 M34 2015
Available from offsite location
- Format:
- Book
- Series:
- Geological Society special publication ; no. 414.
- Geological Society special publication
- Language:
- English
- Subjects (All):
- Magnetic susceptibility.
- Physical Description:
- 283 pages : color and black and white illustrations, maps ; 26 cm.
- Place of Publication:
- London : The Geological Society, 2015.
- Summary:
- Magnetic susceptibility (MS) is a tool frequently used by geologists on sediments or rocks to perform correlations and sea-level or climatic reconstructions. Applied measurements are made on unoriented, bulk samples and bulk MS is mostly influenced by the magnetic mineral content of the rock and often interpreted as influenced by detrital inputs. Magnetic data acquisition is fast and straightforward and this allows the high-resolution sampling needed for palaeoclimatic research (e.g. spectral analysis). However, the link with detrital inputs is not always preserved and the impact of diagenesis on the final MS signal can blur primary information. This volume includes contributions dealing with the origin of the magnetic minerals, and the application of MS as a palaeoenvironmental or palaeoclimatic proxy and also as a tool to provide astronomical calibration in order to improve the chronology of selected time intervals.
- Contents:
- Magnetic susceptibility application: a window onto ancient environments and climatic variations: foreword
- Sedimentary development and magnetic susceptibility evolution of the Frasnian in Western Belgium (Dinant Synclinorium, La Thure section)
- Chemostratigraphy and magnetic susceptibility of the Late Devonian Frasnian-Famennian transition in western Canada and southern China: implications for carbon and nutrient cycling and mass extinction
- Lower Carboniferous ramp sedimentation of the Central Alborz Basin, northern Iran: integrated sedimentological and rock-magnetic studies
- Magnetic susceptibility and facies relationship in Bajocian-Bathonian carbonates from the Aze caves, southeastern Paris Basin, France
- Sedimentology and magnetic susceptibility of recent sediments from New Caledonia
- Petrophysical record of the Late Silurian shallow-water carbonate facies across the Lau Event (Prague Synform, Czech Republic) and dynamic time warping alignment of the magnetic susceptibility logs
- Magnetization carriers of grey to red deep-water limestones in the GSSP of the Givetian-Frasnian boundary (Puech de la Suque, France): signals influenced by moderate diagenetic overprinting
- Magnetic susceptibility and geochemical characterization of an upper Mississippian cyclothemic section Polotnyanyi Zavod, (Moscow Basin, Russia) - A comparison of magnetic susceptibility measurement techniques and ferrimagnetic component analysis from recent sediments in Lake Pepin (USA)
- A climate-driven model using time-series analysis of magnetic susceptibility (x) datasets to represent a floating-point high-resolution geological timescale for the Middle Devonian Eifelian stage
- Forcing factors of the magnetic susceptibility signal in lagoonal and subtidal depositional cycles from the Zachełmie section (Eifelian, Holy Cross Mountains, Poland) - The astronomical calibration of the Givetian (Middle Devonian) timescale (Dinant Synclinorium, Belgium)
- A. Susceptibility and radiometry data used for stratigraphic correlations: case study on Upper Triassic beds in Turkey.
- Notes:
- Includes bibliographical references and index.
- ISBN:
- 9781862397217
- 186239721X
- OCLC:
- 927291610
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