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Characterization of the log lithology of cores LB‐07A and LB‐08A of the Bosumtwi impact structure by using the anisotropy of magnetic susceptibility
Author(s) -
SCHELL Christina,
SCHLEIFER Norbert,
ELBRA Tiiu
Publication year - 2007
Publication title -
meteoritics and planetary science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.09
H-Index - 100
eISSN - 1945-5100
pISSN - 1086-9379
DOI - 10.1111/j.1945-5100.2007.tb01079.x
Subject(s) - geology , breccia , lithology , anisotropy , petrophysics , impact structure , impact crater , texture (cosmology) , mineralogy , geochemistry , petrology , porosity , geotechnical engineering , computer science , image (mathematics) , physics , quantum mechanics , astronomy , artificial intelligence
Abstract— Petrophysical data are commonly used for the discrimination of different lithologies, as the variation in mineralogy, texture, and porosity is accompanied by varying physical properties. A special field of investigation is the analysis of the directional dependence (anisotropy) of the petrophysical properties, which can provide further information on the characteristics of the lithologies, due to the fact that this parameter is different in the various rock‐forming and rock‐changing processes, e.g., deformation or sedimentation. To characterize the rocks in drill cores LB‐07A and LB‐08A, which were drilled into the deep crater moat and central uplift of the Bosumtwi impact structure, Ghana, samples were taken for the study of petrophysical properties. In the present work the magnetic properties of these samples were determined in the laboratory. The results are discussed in relation to the various lithologies represented by this sample suite. The shape and degree of magnetic anisotropy, in combination with the magnetic susceptibility, proved useful in distinguishing between the different lithologies present in the drill cores (polymict lithic breccia, suevite, shale component, and meta‐graywacke). It was possible to correlate layers of high (shale component), intermediate (graywacke, polymict lithic breccia), and low (suevite) anisotropy degree with the lithostratigraphic sequences determined for cores LB‐07A and LB‐08A. The shape of the anisotropy showed that foliation is most dominant within the shale component, whereas lineation is more pronounced in the meta‐graywacke and polymict lithic breccia. An overall increase of the anisotropy degree was observed from core LB‐07A towards core LB‐08A. Thus magnetic anisotropy data provide a useful contribution towards an improved petrophysical characterization of the lithostratigraphic sequences in drillcores from the Bosumtwi impact structure.