Wemmer, Klaus

[["dc.bibliographiccitation.journal","Precambrian Research"],["dc.contributor.author","Oyhantçabal, P."],["dc.contributor.author","Oriolo, S."],["dc.contributor.author","Basei, M. A. S."],["dc.contributor.author","Frei, D."],["dc.contributor.author","Klaus, J."],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.date.accessioned","2022-03-23T08:36:37Z"],["dc.date.available","2022-03-23T08:36:37Z"],["dc.date.issued","2016"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/105045"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Provenance and tectonic affinity of metasedimentary rocks of the western Dom Feliciano Belt in Uruguay: Insights from U-Pb detrital zircon geochronology, Hf isotopes, Sm-Nd whole-rock model ages and geochemical data"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","785"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","International Journal of Earth Sciences"],["dc.bibliographiccitation.lastpage","787"],["dc.bibliographiccitation.volume","96"],["dc.contributor.author","Huckriede, H."],["dc.contributor.author","Wemmer, Klaus"],["dc.date.accessioned","2018-11-07T11:00:06Z"],["dc.date.available","2018-11-07T11:00:06Z"],["dc.date.issued","2007"],["dc.description.abstract","The comment of Martin Oczlon contains some significant contributions to the topics discussed in the article of Huckriede et al. (Int J Earth Sci 93:414-431, 2004). Contrary to Oczlon's comment, the central results of Huckriede et al. (Int J Earth Sci 93:414-431, 2004) are clearly different from the tectonic model of Oczlon (Geol Rundsch 83:20-31, 1994). Additionally, there is no reason for a new interpretation of the K-40/Ar-40 muscovite cooling-ages from allochthonous units."],["dc.identifier.doi","10.1007/s00531-006-0125-3"],["dc.identifier.isi","000247974900012"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/50856"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","1437-3254"],["dc.title","Reply to Oczlon's (2006) comment"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.subtype","letter_note"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","923"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Solid Earth"],["dc.bibliographiccitation.lastpage","951"],["dc.bibliographiccitation.volume","9"],["dc.contributor.author","Koehl, Jean-Baptiste P."],["dc.contributor.author","Bergh, Steffen G."],["dc.contributor.author","Wemmer, Klaus"],["dc.date.accessioned","2020-12-10T18:47:55Z"],["dc.date.available","2020-12-10T18:47:55Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.5194/se-9-923-2018"],["dc.identifier.eissn","1869-9529"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/78944"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Neoproterozoic and post-Caledonian exhumation and shallow faulting in NW Finnmark from K–Ar dating and <i>p</i>∕<i>T</i> analysis of fault rocks"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","141"],["dc.bibliographiccitation.issue","1-4"],["dc.bibliographiccitation.journal","Lithos"],["dc.bibliographiccitation.lastpage","159"],["dc.bibliographiccitation.volume","98"],["dc.contributor.author","Oyhantcabal, Pedro"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Frei, Robert"],["dc.contributor.author","Layer, Paul"],["dc.date.accessioned","2018-11-07T10:58:15Z"],["dc.date.available","2018-11-07T10:58:15Z"],["dc.date.issued","2007"],["dc.description.abstract","In the southernmost Dom Feliciano Belt of Uruguay, highly fractionated calc-alkaline granites, mildly alkaline granites, shoshonitic volcanics, and peralkaline intrusions and volcanics are spatially and temporal associated with the evolution of shear zones. Four representative magmatic unites of this diverse association were petrographic and geochemically investigated: the Solis de Mataojo Complex, a medium to high K2O calc-alkaline granite with signature typical of mature continental arcs and post-collisional settings; the Maldonado granite, highly fractionated calc-alkaline to alkaline, with characteristics that are transitional between both types of series; the Pan de Azucar Pluton, with characteristics typical of post-collisional alkaline granites and the Las Flores shoshonitic basalts. Geochemistry and geotectonic setting point out that slab breakoff was most likely the mechanism associated with the generation of high-K calc-alkaline magmas (Solis de Mataojo and Maldonado) shortly after collision. Extension associated to the formation of molassic basins and emplacement of dolerites and basalt flows with shoshonitic affinity (Las Flores) 15and finally a shift to magmas with alkaline signatures (Pan de Azucar) simultaneous with a second transpressional phase were probably linked with lithospheric thinning through delamination. This evolution took place between 615 and 575 Ma, according to available data. Contrary to previous proposals, which considered this magmatism to represent the root of a continental magmatic are, a post-collisional environment, transitional from orogenic to anorogenic, during transcurrent deformation is proposed. (c) 2007 Elsevier B.V. All rights reserved."],["dc.identifier.doi","10.1016/j.lithos.2007.03.001"],["dc.identifier.isi","000250247200007"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/50436"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0024-4937"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Post-collisional transition from calc-alkaline to alkaline magmatism during transcurrent deformation in the southernmost Dom Feliciano Belt (Braziliano-Pan-African, Uruguay)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","453"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Tectonics"],["dc.bibliographiccitation.lastpage","472"],["dc.bibliographiccitation.volume","32"],["dc.contributor.author","Loebens, Stefan"],["dc.contributor.author","Sobel, Edward R."],["dc.contributor.author","Bense, Frithjof A."],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Dunkl, Istvan"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.date.accessioned","2018-11-07T09:23:49Z"],["dc.date.available","2018-11-07T09:23:49Z"],["dc.date.issued","2013"],["dc.description.abstract","The Sierra de Aconquija and Cumbres Calchaquies in the thick-skinned northern Sierras Pampeanas, NW Argentina present an ideal setting to investigate the tectonically and erosionally controlled exhumation and uplift history of mountain ranges using thermochronological methods. Although these ranges are located along strike of one another, their spatiotemporal evolution varies significantly. Integrating modeled cooling histories constrained by K-Ar ages of muscovite and biotite, apatite fission track data as well as (U-Th)/He measurement of zircon and apatite reveal the structural evolution of these ranges beginning in the late stage of the Paleozoic Famatinian Orogeny. Following localized rift-related exhumation in the central part of the study area and slow erosion elsewhere, growth of the modern topography commenced in the Cenozoic during Andean deformation. The main activity occurred during the late Miocene, with varying magnitudes of rock uplift, surface uplift, and exhumation in the two mountain ranges. The Cumbres Calchaquies is characterized by a total of 5-7km of vertical rock uplift, around 3km of crestal surface uplift, and a maximum exhumation of 2-4km since that time. The Sierra de Aconquija experienced 10-13km of vertical rock uplift, similar to 4-5km of peak surface uplift, and 6-8km of exhumation since around 9Ma. Much of this exhumation occurred along a previously poorly recognized fault. Miocene reactivation of Cretaceous rift structures may explain along-strike variations within these ranges. Dating of sedimentary samples from adjacent basins supports the evolutionary model developed for the mountain ranges."],["dc.identifier.doi","10.1002/tect.20038"],["dc.identifier.isi","000322124300010"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/29676"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0278-7407"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Refined exhumation history of the northern Sierras Pampeanas, Argentina"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","265"],["dc.bibliographiccitation.lastpage","273"],["dc.contributor.author","Steenken, A."],["dc.contributor.author","López de Luchi, M. G."],["dc.contributor.author","Martino, R. D."],["dc.contributor.author","Siegesmund, Siegfried"],["dc.contributor.author","Wemmer, Klaus"],["dc.date.accessioned","2022-03-22T13:47:28Z"],["dc.date.available","2022-03-22T13:47:28Z"],["dc.date.issued","2005"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/104982"],["dc.relation.ispartof","Actas del XVI Congreso Geológico Argentino, La Plata Actas 1"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","SHRIMP dating of the El Peñón granite: a time marker at the turning point between the Pampean and Famatinian cycles within the Conlara Metamorphic Complex (Sierra de San Luis; Argentina)"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Lithosphere"],["dc.bibliographiccitation.volume","2021"],["dc.contributor.author","Schmidt, Susanne Theodora"],["dc.contributor.author","Süssenberger, Annette"],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.editor","Steele-MacInnes, Matt"],["dc.date.accessioned","2021-08-12T07:45:40Z"],["dc.date.available","2021-08-12T07:45:40Z"],["dc.date.issued","2021"],["dc.description.abstract","Abstract This study reports three K/Ar ages on celadonite, a dioctahedral K-Fe mica, in the Proterozoic North Shore Volcanic Group (NSVG) of the Midcontinent Rift in northeastern Minnesota. Celadonite formed during beginning posteruptive, low-temperature conditions at temperatures<100°C and with input of meteoric water. K/Ar ages between 1062±16 Ma and 955.0±12 Ma document a remarkably long posteruptive thermal history of >100 myrs in a thick continental basaltic sequence. In the stratigraphically lower part of the NSVG, celadonite formation occurred at 1062±16 Ma in an amygdule or a vesicle filled with celadonite, while another celadonite amygdule in a stratigraphically higher flow was dated at 1039.4±14 Ma. Both flows are overprinted by a later multistage lower zeolite-phyllosilicate facies assemblage (laumontite-albite-corrensite±chlorite±smectite±prehnite±pumpellyite). In the stratigraphically higher part of the sequence, celadonite crystallization at an amygdule rim is followed by upper zeolite facies conditions (stilbite-heulandite-smectite assemblage) and was dated at 955.0±12.4 Ma. The constrained time frame of 107 myrs indicates a long-lived, probably not continuous and locally occurring, posteruptive thermal alteration process. The data suggest that alteration was depth-controlled and temporally and spatially inhomogeneous and implies the progression of the sequence from a close-to-the-surface alteration mode with input of meteoric water to a burial metamorphic mode and with locally occurring hydrothermal activity due to continuous magmatic activity. Volcanism in the Midcontinent Rift system is supposed to have lasted between 1109 Ma and 1083 Ma based on U/Pb zircon ages. The first crystallization of celadonite is recorded in the lower part of the NSVG and occurred ca. 30 myrs after the emplacement of the Silver Bay aplite intrusion in the upper part of the NSVG. Burial rates are determined to be 0.04 km·Ma-1and 0.10 km·Ma-1. The hydrothermal alteration under low-temperature burial conditions clearly postdates the rift-related alkaline and tholeiitic magmatism of the Midcontinent Rift and overlaps with the depositional window of the sedimentary rocks that overlie the Midcontinent Rift volcanics, as well as crustal-scale fault systems that were active during Grenvillian tectonic uplift after the cessation of magmatic activity."],["dc.description.abstract","Abstract This study reports three K/Ar ages on celadonite, a dioctahedral K-Fe mica, in the Proterozoic North Shore Volcanic Group (NSVG) of the Midcontinent Rift in northeastern Minnesota. Celadonite formed during beginning posteruptive, low-temperature conditions at temperatures<100°C and with input of meteoric water. K/Ar ages between 1062±16 Ma and 955.0±12 Ma document a remarkably long posteruptive thermal history of >100 myrs in a thick continental basaltic sequence. In the stratigraphically lower part of the NSVG, celadonite formation occurred at 1062±16 Ma in an amygdule or a vesicle filled with celadonite, while another celadonite amygdule in a stratigraphically higher flow was dated at 1039.4±14 Ma. Both flows are overprinted by a later multistage lower zeolite-phyllosilicate facies assemblage (laumontite-albite-corrensite±chlorite±smectite±prehnite±pumpellyite). In the stratigraphically higher part of the sequence, celadonite crystallization at an amygdule rim is followed by upper zeolite facies conditions (stilbite-heulandite-smectite assemblage) and was dated at 955.0±12.4 Ma. The constrained time frame of 107 myrs indicates a long-lived, probably not continuous and locally occurring, posteruptive thermal alteration process. The data suggest that alteration was depth-controlled and temporally and spatially inhomogeneous and implies the progression of the sequence from a close-to-the-surface alteration mode with input of meteoric water to a burial metamorphic mode and with locally occurring hydrothermal activity due to continuous magmatic activity. Volcanism in the Midcontinent Rift system is supposed to have lasted between 1109 Ma and 1083 Ma based on U/Pb zircon ages. The first crystallization of celadonite is recorded in the lower part of the NSVG and occurred ca. 30 myrs after the emplacement of the Silver Bay aplite intrusion in the upper part of the NSVG. Burial rates are determined to be 0.04 km·Ma-1and 0.10 km·Ma-1. The hydrothermal alteration under low-temperature burial conditions clearly postdates the rift-related alkaline and tholeiitic magmatism of the Midcontinent Rift and overlaps with the depositional window of the sedimentary rocks that overlie the Midcontinent Rift volcanics, as well as crustal-scale fault systems that were active during Grenvillian tectonic uplift after the cessation of magmatic activity."],["dc.identifier.doi","10.2113/2021/8836546"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/88523"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-448"],["dc.relation.eissn","1947-4253"],["dc.relation.issn","1941-8264"],["dc.title","Posteruptive Thermal History of the Proterozoic Basaltic North Shore Volcanic Group of the Midcontinent Rift: Evidence from K/Ar Data of Celadonite"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","119"],["dc.bibliographiccitation.lastpage","122"],["dc.contributor.author","Martino, R."],["dc.contributor.author","Guereschi, A."],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Lopez de Luchi, M."],["dc.contributor.author","Steenken, A."],["dc.contributor.author","Siegesmund, Siegfried"],["dc.date.accessioned","2022-03-21T16:00:25Z"],["dc.date.available","2022-03-21T16:00:25Z"],["dc.date.issued","2006"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/104976"],["dc.relation.ispartof","Proc. of the V South Ameriacn Symposium on Isotope Geology"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Cooling ages constraints on the tectonic activity of the Los Tuneles shear belt, Eastern Pampeanas ranges of Cordoba, Argentina"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","753"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","International Journal of Earth Sciences"],["dc.bibliographiccitation.lastpage","785"],["dc.bibliographiccitation.volume","100"],["dc.contributor.author","Franke, Wolfgang"],["dc.contributor.author","Doublier, Michael Patrick"],["dc.contributor.author","Klama, Kai"],["dc.contributor.author","Potel, Sebastien"],["dc.contributor.author","Wemmer, Klaus"],["dc.date.accessioned","2018-11-07T08:55:54Z"],["dc.date.available","2018-11-07T08:55:54Z"],["dc.date.issued","2011"],["dc.description.abstract","The Montagne Noire forms the southernmost part of the French Massif Central. Carboniferous flysch sediments and very low-grade metamorphic imprint testify to a very external position in the orogen. Sedimentation of synorogenic clastic sediments continued up to the Vis,an/Namurian boundary (a parts per thousand currency sign320 Ma). Subsequently, the Palaeozoic sedimentary pile underwent recumbent folding and grossly southward thrusting. An extensional window exposes a hot core of Carboniferous HT/LP gneisses, migmatites and granites (Zone Axiale), which was uplifted from under the nappe pile. After the emplacement of the nappes on the Zone Axiale (Variscan D-1), all structural levels shared the same tectonic evolution: D-2 (extension and exhumation), D-3 (refolding) and post-D-3 dextral transtension. HT/LP-metamorphism in the crystalline rocks probably started before and continued after the emplacement of the nappes. Peak metamorphic temperatures were attained during a post-nappe thermal increment (M-2). M-2 occurred during ENE-directed bilateral extension, which exhumed the Zone Axiale and its frame as a ductile horst structure, flanked to the ENE by a Stephanian intra-montane basin. Map patterns and mesoscopic structures reveal that extension in ENE occurred simultaneously with NNW-oriented shortening. Combination of these D-2 effects defines a bulk prolate strain in a \"pinched pull-apart\" setting. Ductile D-2 deformation during M-2 dominates the structural record. In wide parts of the nappes on the southern flank of the Zone Axiale, D-1 is only represented by the inverted position of bedding (overturned limbs of recumbent D-1 folds) and by refolded D-1 folds. U-Pb monazite and zircon ages and K-Ar muscovite ages are in accord with Ar-Ar data from the literature. HT/LP metamorphism and granitoid intrusion commenced already at a parts per thousand yen330 Ma and continued until 297 Ma, and probably in a separate pulse in post-Stephanian time. Metamorphic ages older than c. 300 Ma are not compatible with the classical model of thermal relaxation after stacking, since they either pre-date or too closely post-date the end of flysch sedimentation. We therefore propose that migmatization and granite melt generation were independent from crustal thickening and caused, instead, by the repeated intrusion of melts into a crustal-scale strike-slip shear zone. Advective heating continued in a pull-apart setting whose activity outlasted the emplacement of the Variscan nappe pile. The shear-zone model is confirmed by similar orogen-parallel extensional windows with HT/LP metamorphism and granitoid intrusion in neighbouring areas, whose location is independent from their position in the orogen. We propose that heat transfer from the mantle occurred in dextral strike-slip shear zones controlled by the westward propagating rift of the Palaeotethys ocean, which helped to destroy the Variscan orogen."],["dc.description.sponsorship","Deutsche Forschungsgemeinschaft [Fr 668/24]"],["dc.identifier.doi","10.1007/s00531-010-0512-7"],["dc.identifier.isi","000290036300004"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/23018"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","1437-3262"],["dc.relation.issn","1437-3254"],["dc.title","Hot metamorphic core complex in a cold foreland"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1227"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","International Journal of Earth Sciences"],["dc.bibliographiccitation.lastpage","1246"],["dc.bibliographiccitation.volume","99"],["dc.contributor.author","Oyhantcabal, Pedro"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Layer, Paul"],["dc.date.accessioned","2018-11-07T08:39:45Z"],["dc.date.available","2018-11-07T08:39:45Z"],["dc.date.issued","2010"],["dc.description.abstract","The Sierra Ballena Shear Zone (SBSZ) is part of a high-strain transcurrent system that divides the Neoproterozoic Dom Feliciano Belt of South America into two different domains. The basement on both sides of the SBSZ shows a deformation stage preceding that of the transcurrent deformation recognized as a high temperature mylonitic foliation associated with migmatization. Grain boundary migration and fluid-assisted grain boundary diffusion enhanced by partial melting were the main deformation mechanisms associated with this foliation. Age estimate of this episode is > 658 Ma. The second stage corresponds to the start of transpressional deformation and the nucleation and development of the SBSZ. During this stage, pure shear dominates the deformation, and is characterized by the development of conjugate dextral and sinistral shear zones and the emplacement of syntectonic granites. This event dates to 658-600 Ma based on the age of these intrusions. The third stage was a second transpressional event at about 586 to < 560 Ma that was associated with the emplacement of porphyry dikes and granites that show evidence of flattening. Deformation in the SBSZ took place, during the late stages, under regional low-grade conditions, as indicated by the metamorphic paragenesis in the supracrustals of the country rocks. Granitic mylonites show plastic deformation of quartz and brittle behavior of feldspar. A transition from magmatic to solid-state microstructures is also frequently observed in syntectonic granites. Mylonitic porphyries and quartz mylonites resulted from the deformation of alkaline porphyries and quartz veins emplaced in the shear zone. Quartz veins reflect the release of silica associated with the breakdown of feldspar to white mica during the evolution of the granitic mylonites to phyllonites, which resulted in shear zone weakening. Quartz microstructures characteristic of the transition between regime 2 and regime 3, grain boundary migration and incipient recrystallization in feldspar indicate deformation under lower amphibolite to upper greenschist conditions (550-400A degrees C). On the other hand, the mylonitic porphyries display evidence of feldspar recrystallization suggesting magmatic or high-T solid-state deformation during cooling of the dikes."],["dc.identifier.doi","10.1007/s00531-009-0453-1"],["dc.identifier.isi","000281026800005"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/6761"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/19071"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1437-3254"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","The Sierra Ballena Shear Zone in the southernmost Dom Feliciano Belt (Uruguay): evolution, kinematics, and deformation conditions"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]