Petrophysical properties of the 9-km-deep crustal section at KTB
Petrophysical properties of drill core and drill cuttings samples from both bore holes of the German Continental Deep Drilling Program (KTB) measured at atmospheric pressure and room temperature in the field laboratory are presented, along with data of core samples measured at simulated in situ cond...
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Published in: | Journal of Geophysical Research: Solid Earth Vol. 102; no. B8; pp. 18337 - 18361 |
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Language: | English |
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Blackwell Publishing Ltd
10-08-1997
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Abstract | Petrophysical properties of drill core and drill cuttings samples from both bore holes of the German Continental Deep Drilling Program (KTB) measured at atmospheric pressure and room temperature in the field laboratory are presented, along with data of core samples measured at simulated in situ conditions by other laboratories. Most of the petrophysical properties show a bimodal frequency distribution corresponding to the two main lithologies (gneiss and metabasite), except electrical resitivity and Th/U ratio which are lithology independent (monomodal distribution). Low resistivities are mainly associated with fractures zones enriched in fluids and graphite. The most abundant ferrimagnetic mineral is monoclinic pyrrhotite. Below 8600 m, hexagonal pyrrhotite with a Curie temperature of 260°C is the stable phase. Thus the Curie isotherm of the predominant pyrrhotite was reached (bottom hole temperature about 265°C). The highest values of magnetic susceptibility are linked with magnetite. Microcracks grow due to pressure and temperature release during core uplift. This process continues after recovery and is documented by the anelastic strain relaxation and acoustic emissions. The crystalline rocks exhibit marked reversible hydration swelling. Anisotropy of electrical resistivity, permeability, P and S wave velocity is reduced significantly by applying confining pressure, due to closing of microcracks. Fluids within the microcracks also reduce the P wave velocity anisotropy and P wave attenuation. Anisotropy and shear wave splitting observed in the field seismic experiments is caused by the foliation of rocks, as confirmed by laboratory measurements under simulated in situ conditions. The petrophysical studies provide evidence that microfracturing has an important influence on many physical rock properties in situ. |
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AbstractList | Petrophysical properties of drill core and drill cuttings samples from both bore holes of the German Continental Deep Drilling Program (KTB) measured at atmospheric pressure and room temperature in the field laboratory are presented, along with data of core samples measured at simulated in situ conditions by other laboratories. Most of the petrophysical properties show a bimodal frequency distribution corresponding to the two main lithologies (gneiss and metabasite), except electrical resitivity and Th/U ratio which are lithology independent (monomodal distribution). Low resistivities are mainly associated with fractures zones enriched in fluids and graphite. The most abundant ferrimagnetic mineral is monoclinic pyrrhotite. Below 8600 m, hexagonal pyrrhotite with a Curie temperature of 260°C is the stable phase. Thus the Curie isotherm of the predominant pyrrhotite was reached (bottom hole temperature about 265°C). The highest values of magnetic susceptibility are linked with magnetite. Microcracks grow due to pressure and temperature release during core uplift. This process continues after recovery and is documented by the anelastic strain relaxation and acoustic emissions. The crystalline rocks exhibit marked reversible hydration swelling. Anisotropy of electrical resistivity, permeability,
P
and
S
wave velocity is reduced significantly by applying confining pressure, due to closing of microcracks. Fluids within the microcracks also reduce the
P
wave velocity anisotropy and
P
wave attenuation. Anisotropy and shear wave splitting observed in the field seismic experiments is caused by the foliation of rocks, as confirmed by laboratory measurements under simulated in situ conditions. The petrophysical studies provide evidence that microfracturing has an important influence on many physical rock properties in situ. Petrophysical properties of drill core and drill cuttings samples from both bore holes of the German Continental Deep Drilling Program (KTB) measured at atmospheric pressure and room temperature in the field laboratory are presented, along with data of core samples measured at simulated in situ conditions by other laboratories. Most of the petrophysical properties show a bimodal frequency distribution corresponding to the two main lithologies (gneiss and metabasite), except electrical resitivity and Th/U ratio which are lithology independent (monomodal distribution). Low resistivities are mainly associated with fractures zones enriched in fluids and graphite. The most abundant ferrimagnetic mineral is monoclinic pyrrhotite. Below 8600 m, hexagonal pyrrhotite with a Curie temperature of 260°C is the stable phase. Thus the Curie isotherm of the predominant pyrrhotite was reached (bottom hole temperature about 265°C). The highest values of magnetic susceptibility are linked with magnetite. Microcracks grow due to pressure and temperature release during core uplift. This process continues after recovery and is documented by the anelastic strain relaxation and acoustic emissions. The crystalline rocks exhibit marked reversible hydration swelling. Anisotropy of electrical resistivity, permeability, P and S wave velocity is reduced significantly by applying confining pressure, due to closing of microcracks. Fluids within the microcracks also reduce the P wave velocity anisotropy and P wave attenuation. Anisotropy and shear wave splitting observed in the field seismic experiments is caused by the foliation of rocks, as confirmed by laboratory measurements under simulated in situ conditions. The petrophysical studies provide evidence that microfracturing has an important influence on many physical rock properties in situ. |
Author | Winter, H. Kontny, A. Rauen, A. Popp, T. Soffel, H. C. Zinke, J. Kern, H. Schult, A. Pohl, J. Lienert, M. Nover, G. Berckhemer, H. |
Author_xml | – sequence: 1 givenname: H. surname: Berckhemer fullname: Berckhemer, H. – sequence: 2 givenname: A. surname: Rauen fullname: Rauen, A. – sequence: 3 givenname: H. surname: Winter fullname: Winter, H. – sequence: 4 givenname: H. surname: Kern fullname: Kern, H. – sequence: 5 givenname: A. surname: Kontny fullname: Kontny, A. – sequence: 6 givenname: M. surname: Lienert fullname: Lienert, M. – sequence: 7 givenname: G. surname: Nover fullname: Nover, G. – sequence: 8 givenname: J. surname: Pohl fullname: Pohl, J. – sequence: 9 givenname: T. surname: Popp fullname: Popp, T. – sequence: 10 givenname: A. surname: Schult fullname: Schult, A. – sequence: 11 givenname: J. surname: Zinke fullname: Zinke, J. – sequence: 12 givenname: H. C. surname: Soffel fullname: Soffel, H. C. |
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C. – ident: e_1_2_1_68_1 – ident: e_1_2_1_17_1 doi: 10.1038/367059a0 – ident: e_1_2_1_9_1 doi: 10.1029/96JB02942 – volume: 4 start-page: 215 year: 1994 ident: e_1_2_1_33_1 article-title: In situ seismic velocities versus laboratory measurements: An example from KTB publication-title: Sci. Drill. contributor: fullname: Jahns E. – start-page: 173 volume-title: Contributions to the 8th annual KTB colloquium year: 1995 ident: e_1_2_1_46_1 contributor: fullname: Kontny A. – volume: 4 start-page: 31 year: 1993 ident: e_1_2_1_84_1 article-title: Fabric‐controlled anisotropy of petrophysical properties observed in KTB core samples publication-title: Sci. Drill. contributor: fullname: Siegesmund S. – volume: 4 start-page: 185 year: 1994 ident: e_1_2_1_95_1 article-title: Remanent magnetization of KTB drill cores publication-title: Sci. Drill. contributor: fullname: Worm H. U. – ident: e_1_2_1_11_1 – volume: 9 start-page: 287 year: 1990 ident: e_1_2_1_83_1 article-title: Gefügekundliche Untersuchungen im KTB publication-title: Geowissenschaften contributor: fullname: Siegesmund S. – volume: 85 start-page: 1 year: 1996 ident: e_1_2_1_82_1 article-title: The significance of rock fabrics for the interpretation of geophysical anisotropies publication-title: Geotekt. Forsch. contributor: fullname: Siegesmund S. – ident: e_1_2_1_27_1 doi: 10.1016/0031-9201(91)90100-V – start-page: 433 volume-title: Physical Properties of Rocks, Landolt‐Börnstein, New Series year: 1982 ident: e_1_2_1_24_1 contributor: fullname: Haack U. – ident: e_1_2_1_99_1 doi: 10.1029/JB080i005p00752 |
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Snippet | Petrophysical properties of drill core and drill cuttings samples from both bore holes of the German Continental Deep Drilling Program (KTB) measured at... |
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Title | Petrophysical properties of the 9-km-deep crustal section at KTB |
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