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  • 1
    Book
    Book
    Tübingen : Inst. u. Museum f. Geologie u. Paläontologie d. Univ. Tübingen
    Keywords: Hochschulschrift
    Type of Medium: Book
    Pages: V, 135 S. , graph. Darst.
    ISSN: 0935-4921
    Series Statement: Tübinger geowissenschaftliche Arbeiten 5
    Language: German
    Note: Literaturverz. S. 117 - 129 , Zugl.: Tübingen, Univ., Diss., 1989
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  • 2
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    Enke
    In:  Geologische Rundschau, 78 (1). pp. 197-205.
    Publication Date: 2020-07-30
    Description: Based on sediment physical property data from DSDP/ ODP Legs 78A and 110 (Barbados Ridge Complex), a simple palinspastic reconstruction scheme was employed to study porosity changes during accretion. Undoing the compactional effects caused by imbricate stacking of wedge slices, a synthetic pre-accretion porosity depth profile was developed, which bears strong resemblence to a characteristic profile from a reference drillhole in front of the Barbados accretionary complex. Differences between synthetic and reference profile are interpreted in terms of a semiquantitative estimate of the relative impact of the horizontal stress component on gravitational compaction in accretionary wedge environments. An exponential relationship between depth and porosity divergence for distinct lithologic units is evident. The defined relationship facilitates the analysis of deformational behavior of accreted sediments in general.
    Type: Article , PeerReviewed
    Format: text
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  • 3
    Publication Date: 2019-09-23
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 4
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    Unknown
    In:  [Talk] In: DMG-GV-DGG-Tagung GEO2003, 22.- 25.09.2003, Bochum, Germany .
    Publication Date: 2019-09-23
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 5
    Publication Date: 2019-09-23
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 6
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    Unknown
    In:  Proceedings of the Ocean Drilling Program: Scientific Results, 171A . pp. 1-29.
    Publication Date: 2016-10-25
    Description: In the northern Barbados accretionary wedge, several Deep Sea Drilling Project (DSDP) and Ocean Drilling Program (ODP) legs (DSDP Leg 78 and ODP Legs 110, 156, and 171A) targeted the décollement and the seaward extension of the décollement, the proto-décollement. During Leg 171A, the logging while drilling (LWD) technique was used to determine the physical properties variations along a profile across the deformation front. Because of the unstable borehole conditions in accretionary wedges, LWD is the most effective method for the measurements of physical properties in these poorly consolidated sediments. LWD data are acquired just above the drill bit a few minutes after the formation has been drilled, yielding measurements as close to in situ conditions as possible. The large amount of LWD data and the demand for a quick, objective, and reliable evaluation calls for the application of multivariate statistical methods. The multivariate factor analysis is a method of reducing the amount of logging data while giving them a new integrated meaning with no loss of important information, resulting in factor logs that are helpful tools for further interpretation. The cluster analysis of the two or three most significant factors proved to be a useful and objective method to identify and confirm significant logging units. The main objective of the application of multivariate statistical methods in this study is twofold. First, Leg 171A was a stand-alone logging leg, where no cores were retrieved. The factor analysis was used as an objective tool for a classification of the drilled sequences based on their physical and chemical properties. The new factor logs mirror the basic processes behind the measured geophysical properties and make them easier to interpret. Second, in the succeeding cluster analysis, similar geophysical properties are grouped into one cluster, reflecting one logging unit. These objectively defined logging units can be compared to statistical electrofacies, which are helpful in differentiating lithologic characterizations. In particular for LWD measurements, the multivariate statistical methods of factor and cluster analysis are helpful tools for a fast, reliable, and objective definition of logging units, which should be considered for future legs.
    Type: Article , NonPeerReviewed
    Format: text
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  • 7
    Publication Date: 2020-05-20
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 8
    Publication Date: 2020-05-11
    Description: Gas hydrates were recovered from a mud diapir (Mound 11) located on the southern continental slope off Costa Rica at a water depth of about 1000 m during expedition M54/2 with RV METEOR in September 2002. A massive layer of solid methane gas hydrate was retrieved from the base of a gravity corer at a sediment depth of 2 m. Several mound-shaped and carbonate-covered mud diapirs were previously discovered off Costa Rica and Nicaragua during the ongoing research within the framework of the Sonderforschungsbereich 574 "Volatiles and Fluids in Subduction Zones" but solid hydrates were recovered only from Mound 11. This structure has a diameter of about 300 m and protrudes the surrounding seafloor by about 20 m. The seamount sits on approximately 1 km of hemipelagic sediment disrupted by normal faults, which could provide fluid and mass transport pathways from greater depth to the sea floor. Video observations of Mound 11 revealed the presence of authigenic carbonates and bacterial mats indicating methane-charged fluids reaching the sediment surface. Water sampling and gas chromatographic analyses showed methane enrichments in the overlying bottom water confirming the release of methane. In-situ temperature measurements indicated elevated heat flow within the hydrate-bearing sediment strata. Pore fluids recovered from the mound were strongly depleted in dissolved chloride and enriched in boron indicating a deep origin of rising fluids and gases. The results of the ongoing isotopic analysis of gas hydrates and pore waters will be used to further constrain the source of methane-rich fluids.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 9
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    In:  [Talk] In: EGS-AGU-EUG Joint Assembly 2003, 06.-11.04.2003, Nice, France .
    Publication Date: 2020-05-26
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 10
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    Institut und Museum für Geologie und Paläontologie der Universität Tübingen
    In:  Tübinger Geowissenschaftliche Abhandlungen A, 5 . Institut und Museum für Geologie und Paläontologie der Universität Tübingen, Tübingen, V, 135 pp.
    Publication Date: 2017-11-06
    Description: Der Einfluß lateralen Stresses auf die mechanische Diagenese von marinen Sedimenten kann mithilfe sedimentphysikalischer Daten quantifiziert werden. Beispielhaft wurde dies anhand von Daten aus dem Deep Sea Drilling Project (DSDP) und Ocean Drilling Project (ODP) für den Akkretionskeil des Barbados Ridge Complex durchgeführt. Die Untersuchung erfolgte in drei Schritten. (1) In einer statistischen Untersuchung der umfangreichen sedimentologischen und sedimentphysikalischen Datenbank des DSDP wurden tief enabhängige Funktionen der mechanischen Diagenese für eine Reihe von lithologischen Standardtypen definiert. Diese, als Referenzgröße zur Quantifizierung der tektonischen KonsoHdation in einem rezenten Akkretionskeil benötigten Funktionen, wurden in erster Linie für pelitische und psammitische Sedimente mit geringen Karbonatgehalten entwickelt. Zwei verschiedene Verfahren zur Auswahl von entsprechenden Datensätzen werden beschrieben und die Ergebnisse der statistischen Untersuchung mit den in der Literatur beschriebenen Funktionen verglichen. (2) Die entwickelten Typfunktionen wurden bei der Durchführung eines palinspastischen Rekonstruktionsverfahrens benutzt, mit dem die Entwicklung sedimentphysikalischer Parameter während der initialen Deformationsphase in rezenten Akkretionssystemen modelliert werden konnte. Diese Untersuchung basierte im wesentlichen auf sedimentphysikalischen Daten der DSDP- und ODP-Legs 78A und J 10 (Barbados Ridge Komplex, Kleine Antillen). Durch palinspastische Entzerrung der imbrikierten Schuppung und stratigraphische Rekonstruktion akkretierter "thrust slices" im untersuchten Bereich, entsprechender Relozierung der zugehörigen sedimentphysikalischen Daten und dekompaktive Anpassung an die rekonstruierte Position konnte ein synthetisches prä-akkretionäres Profil der ursprünglichen Porosität rechnerisch modelliert werden. (3) Der Vergleich dieses synthetischen Porositäts-Tiefen-Profils mit charakteristischen Referenzprofilen aus undeformierten Sequenzen unmittelbar vor der Deformationsf ront zeigt eine systematische, lithologisch bestimmte Divergenz. Durch Überarbeitung des Rekonstruktionsverfahrens mithilfe von Stress-PorositätsBeziehungen konnte der relative und absolute Einfluß der lateralen Stresskomponente auf die Konsolidation hemipelagischer Sedimente in diesem Teil des konvergenten Plattenrandes quantifiziert werden.
    Type: Report , NonPeerReviewed
    Format: text
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