Leiss, Bernd

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[["dc.bibliographiccitation.firstpage","131"],["dc.bibliographiccitation.lastpage","168"],["dc.contributor.author","Tanner, D. C."],["dc.contributor.author","Leiss, Bernd"],["dc.contributor.author","Vollbrecht, A."],["dc.contributor.editor","Kirnbauer, T."],["dc.date.accessioned","2022-03-07T15:49:30Z"],["dc.date.available","2022-03-07T15:49:30Z"],["dc.date.issued","2013"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/104442"],["dc.relation.ispartof","Geologische Exkursionen in die Region um Göttingen und weitere wissenschaftliche Beiträge"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Strukturgeologie des Leinetalgrabens"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.contributor.author","Walter, J. M."],["dc.contributor.author","Leiss, Bernd"],["dc.contributor.author","Weber, K."],["dc.date.accessioned","2020-09-22T09:56:07Z"],["dc.date.available","2020-09-22T09:56:07Z"],["dc.date.issued","2004"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/67879"],["dc.notes.preprint","yes"],["dc.relation.conference","32nd International Geological Congress (32IGC)"],["dc.relation.eventlocation","Florence, Italy"],["dc.relation.eventstart","2004-08"],["dc.relation.iserratumof","yes"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Brittle and ductile deformation of graphite bearing marbles in high strain zones of the central Damara Belt, Namibia"],["dc.type","conference_paper"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.lastpage","5"],["dc.contributor.author","Leiss, Bernd"],["dc.contributor.author","Romanov, D."],["dc.contributor.author","Wagner, Bianca"],["dc.date.accessioned","2022-03-24T12:14:26Z"],["dc.date.available","2022-03-24T12:14:26Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.3997/2214-4609.202021044"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/105117"],["dc.notes.preprint","yes"],["dc.relation.conference","1st Geoscience & Engineering in Energy Transition Conference"],["dc.relation.eventstart","2020-11"],["dc.relation.iserratumof","yes"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Risks and Challenges of the Transition to an Integrated Geothermal Concept for the Göttingen University Campus"],["dc.type","conference_paper"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1227"],["dc.bibliographiccitation.journal","Journal of Applied Crystallography"],["dc.bibliographiccitation.lastpage","1237"],["dc.bibliographiccitation.volume","44"],["dc.contributor.author","Luque, A."],["dc.contributor.author","Leiss, Bernd"],["dc.contributor.author","Alvarez-Lloret, P."],["dc.contributor.author","Cultrone, G."],["dc.contributor.author","Siegesmund, Siegfried"],["dc.contributor.author","Sebastian, E."],["dc.contributor.author","Cardell, C."],["dc.date.accessioned","2018-11-07T08:49:30Z"],["dc.date.available","2018-11-07T08:49:30Z"],["dc.date.issued","2011"],["dc.description.abstract","Marble has historically been used as an ornamental stone because of its aesthetic appeal, ease of polishing and ex;cellent physical properties. One of the main factors affecting the durability of marbles is their thermal behaviour. Although marble is used extensively in Spain as a building and decorative material, little research has been done into its thermal behaviour. In this work, the textural and microstructural properties of seven calcitic and dolomitic marbles from Andalusia (southern Spain) were characterized to assess how these properties affect their thermal response. Rock fabric properties (grain morphology, boundaries and micro-crack populations) were studied by polarized microscopy and lattice preferred orientation using X-ray texture goniometry. Elastic properties were measured by ultrasound, thermal properties were determined by a six-rod dilatometer (thermal expansion) and the opening of micro-cracks was observed using environmental scanning electron microscopy. For each marble, thermal coefficients of calcite and dolomite crystals were calculated using thermo-X-ray diffraction, a novel application to characterize historic marbles. The results show that marble thermal expansion coefficients are related to preferred crystallographic orientation, which can help to identify the directions along which decay occurs. The results also show for the first time that the thermal expansion coefficient of the main components of marble, i.e. calcite and dolomite, is specific to each marble, and plays a key role in their different thermal behaviours. Thermal properties also depend on mineral composition, the existence of micro-cracks and hydric properties."],["dc.identifier.doi","10.1107/S0021889811036910"],["dc.identifier.isi","000297279800014"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/21473"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0021-8898"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Potential thermal expansion of calcitic and dolomitic marbles from Andalusia (Spain)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","84"],["dc.bibliographiccitation.journal","Geowissenschaftliche Mitteilungen"],["dc.bibliographiccitation.lastpage","85"],["dc.bibliographiccitation.volume","45"],["dc.contributor.author","Walter, J."],["dc.contributor.author","Leiss, Bernd"],["dc.contributor.author","Reitner, J."],["dc.contributor.author","Siegesmund, Siegfried"],["dc.contributor.author","Vollbrecht, A."],["dc.date.accessioned","2020-09-18T08:19:15Z"],["dc.date.available","2020-09-18T08:19:15Z"],["dc.date.issued","2011"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/67721"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Klaus Weber 1936 - 2010"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","obituary_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","527"],["dc.bibliographiccitation.issue","2/3"],["dc.bibliographiccitation.journal","Zeitschrift der Deutschen Geologischen Gesellschaft"],["dc.bibliographiccitation.lastpage","545"],["dc.bibliographiccitation.volume","152"],["dc.contributor.author","Leiss, Bernd"],["dc.contributor.author","Lapp, M."],["dc.date.accessioned","2022-03-10T12:21:08Z"],["dc.date.available","2022-03-10T12:21:08Z"],["dc.date.issued","2001"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/104636"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Fluid-controlled microstructural and textural evolution of a calcite-dolomite marble from the western Erzgebirge in Germany"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","87"],["dc.bibliographiccitation.lastpage","102"],["dc.contributor.author","Friedel, C.-H."],["dc.contributor.author","Blanke, H."],["dc.contributor.author","Leiss, Bernd"],["dc.contributor.author","Patzschke, M."],["dc.contributor.author","Wagner, Bianca"],["dc.contributor.editor","Röhling, H.-G."],["dc.date.accessioned","2022-03-24T13:05:47Z"],["dc.date.available","2022-03-24T13:05:47Z"],["dc.date.issued","2015"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/105131"],["dc.publisher.place","Hannover"],["dc.relation.ispartof","GeoBerlin 2015. DYNAMISCHE ERDE - von Alfred Wegener bis heute und in die Zukunft. Exkursionsführer/Excursion guide"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Geologie und Tektonik der Allertalsalzstruktur im ehemaligen Salzbergwerk Morsleben"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1474"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","Acta Geologica Sinica - English Edition"],["dc.bibliographiccitation.lastpage","1487"],["dc.bibliographiccitation.volume","84"],["dc.contributor.author","Cao Shuyun, Cao Shuyun"],["dc.contributor.author","Liu Junlai, Liu Junlai"],["dc.contributor.author","Leiss, Bernd"],["dc.contributor.author","Zhao Chunqiang, Zhao Chunqiang"],["dc.date.accessioned","2018-11-07T08:46:51Z"],["dc.date.available","2018-11-07T08:46:51Z"],["dc.date.issued","2010"],["dc.description.abstract","The Ailao Shan-Red River fault zone is the boundary between the Yangtze block to the northeast and the Indochina block to the southwest. It is an important tectonic zone due to its role in the southeastward extrusion of the Indochina block during and subsequent to the Indian-Eurasian collision. Diancang Shan (DCS) high-grade metamorphic complex, located at the northwest extension along the Ailao Shan-Red River (ASRR) shear zone, is a representative metamorphic complex of the ASRR tectonic belt. Structural and microstructural analysis of sheared rocks in the high-grade metamorphic rocks reveals that they are coherent with solid-state high-temperature ductile deformation, which is attributed to left-lateral shearing along the ASRR shear zone. New LA-ICP-MS zircon U-Pb geochronological and microstructural studies of the post-kinematic granitic plutons provide a straightforward time constraint on the termination ductile left-lateral shearing and exhumation of the metamorphic massif in the ASRR shear zone. It is suggested that the left-lateral shearing along the ASRR shear zone ended at ca. 21 Ma at relative lower-temperature or decreasing temperature conditions. During or after the emplacement of the young dikes at ca. 21 Ma, rapid brittle deformation event occurred, which makes the DCS massif start fast uplift/exhumation and cooling to a shallow crustal level."],["dc.identifier.doi","10.1111/j.1755-6724.2010.00342.x"],["dc.identifier.isi","000285753000014"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/20796"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1000-9515"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","New Zircon U-Pb Geochronology of the Post-kinematic Granitic Plutons in the Diancang Shan Metamorphic Massif along the Ailao Shan-Red River Shear Zone and Its Geological Implications"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","259"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Zeitschrift der Deutschen Geologischen Gesellschaft"],["dc.bibliographiccitation.lastpage","274"],["dc.bibliographiccitation.volume","150"],["dc.contributor.author","Leiss, Bernd"],["dc.contributor.author","Ullemeyer, K."],["dc.date.accessioned","2022-03-24T10:11:40Z"],["dc.date.available","2022-03-24T10:11:40Z"],["dc.date.issued","1999"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/105112"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Texture characterisation of carbonate rocks and some implications for the modeling of physical anisotropies, derived from idealized texture types"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]