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  • 11
    Publication Date: 2021-03-29
    Description: The North Equatorial Panafrican belt is constituted by orthogneissified metamorphic and magmatic sets linked to tectonometamorphic events of the neoproterozoic orogeny. This belt whose formations are situated in the North of the congo craton is divided into three distinct geodynamic domains: a southern domain, a northern domain and a central domain. The deformation and metamorphism relationships are a function of the different geodynamic domains of the belt. The central domains, to which belongs the Banefo region, is affected by large strike-slip faults among which is the central cameroonian shear zone. This domain is marked out by numerous syntectonic granitoids. At Banefo (NE Bafoussam, West Cameroon), those massifs are mainly constituted by mylotinised orthogneisses and granites of various degrees. The country rock is made up of gneiss and amphibolite. In the Banefo massifs, the orthogneiss is the least deformed petrographic unit. It shows a heterogranular granoblastic texture with a mineral assemblage formed by quartz, K-feldspars, biotite, etc., within the orthogneiss, remains of magmatic fluidality can still be observed marked by feldspar megacrystal. Field observations reveal a net progression of the intensity of deformation of orthogeisses to ultramylotinised granites having an identical chemical composition as the orthogneisses...
    Description: conference
    Keywords: 551 ; VKA 200 ; VAE 140 ; VAE 850 ; VKB 270 ; VEP 500 ; Gefügekunde der Gesteine ; Gesteinsdeformation {Strukturgeologie} ; Festländische Lineamente {Geologie} ; Produkte mechanischer Deformation {Petrologie} ; Kamerun {Geologie} ; Kamerun-Linie ; Granitgneis ; Mylonit ; Deformation 〈Geologie〉
    Language: German
    Type: anthologyArticle , publishedVersion
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  • 12
    Publication Date: 2021-03-29
    Description: Die Insel Kreta bildet den südlichen Rand der externen Helleniden, welche üblicherweise in zwei Deckenstapel untergliedert werden: Die unteren Decken (Plattenkalk und Phyllit-Quarzit- Einheit) sind durch eine alpidische HP-Metamorphose (Oligozän/Miozän) gekennzeichnet (Seidel et al. 1982, Jolivet et al. 1996), welche im Hangenden bislang nicht nachgewiesen wurde. Die Oberen Decken (i.w. Tripolitza- und Pindos-Einheit) bestehen aus karbonatischen Gesteinen und sind für eine petrologische PT-Abschätzung ungeeignet. Aufgrund des Gesteinshabitus wurden sie als unmetamorph eingestuft. Schlußfolgernd wird der Kontakt der beiden Stapel seit etwa zwanzig Jahren als krustales Megadetachment (‚Kreta- Detachment‘) aufgefaßt (Jolivet et al. 1996, Fassoulas et al. 1994, Kilias et al. 1994), wobei Versatzbeträge von über 100km angenommen werden (Ring et al. 2001, 2001). Ziel dieser Arbeit ist es Gemeinsamkeiten und Unterschiede der unmittelbar an das Detachment angrenzenden Einheiten herauszuarbeiten, um Rückschlüsse auf die tatsächliche Signifikanz der Störungszone zu ziehen.
    Description: conference
    Keywords: 551 ; VEF 000 ; VAE 140 ; VAE 400 ; VKA 200 ; VKB 292 ; VKB 250 ; Südeuropa und Mittelmeergebiet {Geologie} ; Gesteinsdeformation {Strukturgeologie} ; Tektogenese {Geologie} ; Gefügekunde der Gesteine ; Metamorphe Komplexe, übriges Europa {Petrologie} ; Metasedimente {Petrologie} ; Kreta ; Abscherung ; Deformation 〈Geologie〉 ; Alpidische Gebirgsbildung ; Metamorphose 〈Geologie〉
    Language: German
    Type: anthologyArticle , publishedVersion
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  • 13
    Publication Date: 2021-03-29
    Description: During impact, rocks at the surface and accessible depths encounter extreme conditions. The hydrostatic component of the shock wave-associatedstress, the so-called shock pressure, canreach several tens of GPa in the central part of the structure. The shock crust and its comprehensive experimental calibration. Two distinct types of quartz microstructure in charnockitic target rocks and quartz veins of the Charlevoix impact structure are compared and contrasted in order to distinguish shock-induced microstructures that indicate a high hydrostatic stress component of the shock wave-associated stress from those that indicate a high deviatoric component, as well as associated microstructures that were generated during post-shock relaxation...
    Description: conference
    Keywords: 551 ; VKA 200 ; VAE 140 ; VHB 400 ; VKB 280 ; VEB 128 ; Gefügekunde der Gesteine ; Gesteinsdeformation {Strukturgeologie} ; Oxide und Hydroxide {Mineralogie} ; Impaktgesteine {Petrologie} ; Saxothuringikum {Geologie} ; Charlevoix 〈Quebec〉 ; Impaktstruktur ; Impaltmetamorphes Gestein ; Deformation 〈Geologie〉 ; Quarz ; Mikrostruktur
    Language: German
    Type: anthologyArticle , publishedVersion
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  • 14
    Publication Date: 2021-03-29
    Description: Granitic gneisses of the Central Aar Granite host a shear zone network that formed at greenschist facies conditions. The work area is located in the Bächlital (Grimsel area, Central Switzerland) and was chosen for the analysis of shear zones because of the weakly anisotropic fabric of the host gneisses. Contrary to previous publications (e.g. Choukroune & Gapais, 1983), none of these host rocks are undeformed. They contain a penetrative foliation (S1) that strikes consistently ENE-WSW with a steep dip of around 70° to the south. This foliation is overprinted by the aforementioned shear zone network, which was the main focus of this study...
    Description: conference
    Keywords: 551 ; VAE 140 ; VKA 200 ; VKB 291 ; VEB 168 ; VKB 230 ; VKB 270 ; Gesteinsdeformation {Strukturgeologie} ; Gefügekunde der Gesteine ; Metamorphe Komplexe, Alpen {Petrologie} ; Schweizer Alpen {Geologie} ; Metamorphite aus sauren bis intermediären Edukten {Petrologie} ; Produkte mechanischer Deformation {Petrologie} ; Aarmassiv ; Scherzone ; Granitgneis ; Feldspäte ; Deformation 〈Geologie〉
    Language: German
    Type: anthologyArticle , publishedVersion
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  • 15
    Publication Date: 2021-03-29
    Description: Halite veins hosted in clastic sedimentary rocks are frequently observed next to evaporite layers. Their microstructure can be enhanced by gamma irradiation and etching, which can be used to infer the deformation mechanism of halite (e.g. Howard & Kerr 1960, Schleder & Urai 2005). In this study, we present results from gammadecorated vein microstructures of fibrous halite veins hosted in claystone.
    Description: conference
    Keywords: 551 ; VAE 160 ; VKA 200 ; VAE 140 ; Salztektonik {Strukturgeologie} ; Gefügekunde der Gesteine ; Gesteinsdeformation {Strukturgeologie} ; Steinsalz ; Mikrogefüge ; Deformation 〈Geologie〉 ; Salztektonik
    Language: German
    Type: anthologyArticle , publishedVersion
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  • 16
    Publication Date: 2021-03-29
    Description: Archaische Granitoide und paläoproterozoische Metasedimente der Huronian Supergroup werden von dem schüsselförmigen und partiell erodierten 1.85 Ga alten Impaktschmelzkomplex der Sudbury-Impaktstruktur überlagert. Huronische Metasedimente und deren basaler Kontakt zum granitoiden Grundgebirge stehen in einer Entfernung bis zu 15km von dem lagigen Komplex und um diesen herum steil. Obwohl diese Steilstellung durch die Bildung eines impakt-induzierten Zentralberges erklärt werden kann, ist unklar, ob orogene Verformung vor dem Impakt an der Steilstellung beteiligt war. Um hierüber Aufschluss zu gewinnen, wurden die basalen Huronischen Einheiten, insbesondere die karbonatische Espanola Formation und deren benachbarte Metakonglomerate und Metasandsteine, nordöstlich des Impaktschmelzkomplexes strukturell untersucht. Aufgrund er Nähe der metasedimentären Einheiten zu dem 2,5km mächtigen Schmelzkomplex wurde daher auch dessen möglicher thermischer Einfluss auf die Metasedimente untersucht...
    Description: conference
    Keywords: 551 ; VKB 280 ; VKB 295 ; VAE 140 ; VEV 127 ; VKA 200 ; Impaktgesteine {Petrologie} ; Metamorphe Komplexe, Nordamerika {Petrologie} ; Gesteinsdeformation {Strukturgeologie} ; Ontario {Geologie} ; Gefügekunde der Gesteine ; Sudbury 〈Ontario. Region〉 ; Mehrfachringbassin ; Proterozoikum ; mpaktmetamorphes Gestein ; Karbonatgestein ; Deformation 〈Geologie〉
    Language: German
    Type: anthologyArticle , publishedVersion
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  • 17
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    Universitätsverlag Göttingen
    Publication Date: 2021-03-29
    Description: When viewed as ideal elastic cracks, seismogenic faults are often modeled as decreases from the host rock to the boundary between the core and the damage zone. mode II or mode III cracks in semiinfinite elastic bodies or half spaces. These models normally assume the rock to be homogeneous and isotropic. Such assumptions may be justified and necessary when using closed-form analytical solutions for fault displacement. They are not justified, however, when we attempt to understand fault-displacement profiles along earthquake rupture sites or in paleofault studies. This follows because crustal segments hosting faults are, as a rule, not homogeneous and isotropic, but rather heterogeneous and anisotropic. In particular, the fault rocks commonly form layers or units parallel with the fault plane. Also, the mechanical properties of the rocks next to the fault change as the fault develops (Gudmundsson 2004). During repeated earthquakes in a seismogenic fault zone, two main rock units develop around the fault plane. One unit is the core, located next to the fault plane and normally composed of soft (low Young’s modulus) breccia, gouge, and other cataclastic rocks. The other unit is the damage zone, containing some cataclastic rocks but characterized by fractures of various types...
    Description: conference
    Keywords: 551 ; VAE 140 ; VAE 150 ; Gesteinsdeformation {Strukturgeologie} ; Strukturelle Erscheinungen {Strukturgeologie} ; Bruchzone ; Deformation 〈Geologie〉 ; Verwerfung ; Modellierung
    Language: German
    Type: anthologyArticle , publishedVersion
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  • 18
    Publication Date: 2021-03-29
    Description: The anisotropy of magnetic susceptibility (AMS) is a time-efficient method to describe crystallographic preferred orientations of rocks and has been applied in a wide field of sedimentary, metamorphic and magmatic geology. The method, however, suffers from limitations which mainly result from the interference of diamagnetic, paramagnetic and ferromagnetic fabrics (de Wall 2005) — the term ferromagnetism is used in a wider sense here, including e.g. ferrimagnetism. The AMS is an integral parameter which describes a crystallographic preferred orientation as an ellipsoid. The quantitative correlation of the AMS with the crystallographic preferred orientations should help to allow a closer view at the applicability and the limitations of the AMS analysis (see also Schmidt et al. 2006 a, b)... The results of this study are based on a large variety of fabric types of carbonate-mica marbles and mylonites, i.e. varying mica content, grain sizes, grain shapes, types and intensities of the crystallographic preferred orientation. The presented first correlations of the AMS and CPO for the single mineral phases in general demonstrate a good matching. Regarding the comparison of texture types and the AMS, limitations are possible. While single c-axis maxima and girdle-like c-axis distributions can be also distinguished by the AMS, it is obvious that distinguishing between these types and the double c-axis type is not possible at the present stage.
    Description: conference
    Keywords: 551 ; TOT 310 ; VKA 200 ; VAE 140 ; VEF 200 ; VER 200 ; VKB 270 ; VAE 120 ; Gesteinsmagnetismus {Geophysik} ; Gefügekunde der Gesteine ; Gesteinsdeformation {Strukturgeologie} ; Italien {Geologie} ; Namibia {Geologie} ; Produkte mechanischer Deformation {Petrologie} ; Methodik {Strukturgeologie} ; Apuaner Alpen ; Damara Orogen ; Karbonatgestein ; Deformation 〈Geologie〉 ; Magnetische Suszeptibilität ; Kristallorientierung ; Korrelationsanalyse
    Language: German
    Type: anthologyArticle , publishedVersion
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  • 19
    Publication Date: 2021-03-29
    Description: The island of Serifos is located in the Western Cyclades within the Attic- Cycladic metamorphic belt. It represents the westward continuation of an arcuate belt of Metamorphic Core Complexes with intrusions of late syn-post tectonic intrusions younging from East (e.g. Naxos main activity ca. 12Ma) to West (e.g. Serifos with 9–8Ma). In scientific discussions the dominance of probably continuous extension since ca. 30Ma (e.g. Jolivet & Faccenna, 2000) and the presence of Metamorphic Core Complexes (Lister et al. 1984) is accepted. The speculated roll-back of the subducting plate possibly started due to the slowing down of absolute plate convergence rate between Africa and Eurasia. This model is attractive, because it would also explain the shift from a compressional Andean-type regime to an extensional Mariana-type regime (Jolivet & Faccenna 2000). Contrary to the kinematic directions reported from the Central and Eastern Cyclades, the movement of the hanging wall of the Serifos Metamorphic Core Complex is south directed. The island’s main part is occupied by an undeformed granodiorite. Early granitic intrusions intruded into low-grade M2-crystalline rocks that have been overprinted to as high as amphibolite facies conditions due to contact metamorphism. Parts of these rocks (gneisses and amphibolites) as well as the early intrusions are deformed to mylonites (Grasemann et al. 2004).
    Description: conference
    Keywords: 551 ; VEF 300 ; VKB 292 ; VKB 270 ; VAE 140 ; Griechenland und griechische Inseln {Geologie} ; Metamorphe Komplexe, übriges Europa {Petrologie} ; Produkte mechanischer Deformation {Petrologie} ; Gesteinsdeformation {Strukturgeologie} ; Serifos ; Scherzone ; Mylonit ; Deformation 〈Geologie〉
    Language: German
    Type: anthologyArticle , publishedVersion
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  • 20
    Publication Date: 2021-03-29
    Description: Das Untersuchungsgebiet liegt im Übergangsbereich zwischen den Svekofenniden und der Transskandinavischen Magmatischen Zone, welcher als Teil einer Paläoproterozoischen E- bis NE-abtauchenden Subduktionszone interpretiert wird (z.B. Beunk & Page 2001). Im heutigen tiefkrustalen Erosionsniveau sind im Wesentlichen mehrere Generationen von Granitioden aufgeschlossen, die etwa im Zeitraum 1850–1650Ma (z.B. Åhäll & Larson 2000) in die zuvor gefalteten Metasedimente und Metavulkanite der paläo-Proterozoischen Västervik- Formation intrudierten. Dabei kam es, in Abhängigkeit von der primären Lithologie der Schichtenfolge, zu unterschiedlichen Formen kontaktmetamorpher und migmatischer Überprägungen bis hin zur Bildung anatektischer Granite. Innerhalb dieser migmatisch/ anatektischen Bereiche stellen Metabasite und Metaquarzite schmelzresistente Horizonte der ursprünglichen Abfolge dar. Nordwestlich von Västervik zeigen entsprechende Metaquarzite lokal komplexe, z.T. nicht-zylindrische Falten im m- bis 10er m-Maßstab, die sich deutlich von der einfacheren, großmaßdimesionierten Faltung in dieser Region abheben. Aufgrund von ersten Ergebnissen einer Vorstudie und einer Diplomkartierung wird angenommen, dass diese Strukturen durch Intrusionen von Mini-Lakkolithen in tiefere Niveaus der Västervik-Formation erzeugt wurden...
    Description: conference
    Keywords: 551 ; VAE 150 ; VAE 400 ; VAE 140 ; VKB 292 ; VKB 250 ; VKB 220 ; Strukturelle Erscheinungen {Strukturgeologie} ; Tektogenese {Geologie} ; Gesteinsdeformation {Strukturgeologie} ; Metamorphe Komplexe, übriges Europa {Petrologie} ; Metasedimente {Petrologie} ; Kontaktmetamorphe und metasomatische Gesteine {Petrologie} ; Svekofenniden ; Västervik 〈Region〉 ; Proterozoikum ; Aureole 〈Geologie〉 ; Metasediment ; Quarzit ; Faltung 〈Geologie〉 ; Deformation 〈Geologie〉
    Language: German
    Type: anthologyArticle , publishedVersion
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