Hueck, Mathias

[["dc.bibliographiccitation.journal","International Journal of Earth Sciences"],["dc.contributor.author","Silva Lara, Hernan"],["dc.contributor.author","Siegesmund, S."],["dc.contributor.author","Oriolo, S."],["dc.contributor.author","Hueck, M."],["dc.contributor.author","Wemmer, K."],["dc.contributor.author","Basei, M. A. S."],["dc.contributor.author","Oyhantçabal, P."],["dc.date.accessioned","2022-09-01T09:49:18Z"],["dc.date.available","2022-09-01T09:49:18Z"],["dc.date.issued","2022"],["dc.description.abstract","Abstract\n \n Some recent models challenge the position and extension of the assumed oceanic basins formed through the break-up of Rodinia, and the tectonic processes involved in the Gondwana assembly, making the investigation of the Early Neoproterozoic record of great relevance. Within the South-American Atlantic margin, the Punta del Este Terrane (PET) of the Dom Feliciano Belt (DFB) comprises a unique Tonian to Ediacaran record, and has a strategic position to reconstruct spatio-temporal relationships with the southern African orogenic belts. Novel zircon U–Pb and Lu–Hf data from the PET basement orthogneisses display Tonian magmatic ages (805–760 Ma) and Hf isotopic signatures indicative of mainly crustal/metasedimentary sources, (Nd T\n DM\n ages: 2.2–1.9 Ga, and εHf(t): − 12 to − 4). The basement paragneisses yielded late Paleoproterozoic to Neoproterozoic U–Pb ages, but dominantly positive εHf(t) values. The presented results confirm the correlation of the PET with the Coastal Terrane of the Kaoko Belt, and discard the idea of the Nico Pérez Terrane as a source. Detrital zircon U–Pb and Lu–Hf data from the Rocha Formation yielded a main peak at ca. 660 Ma, with the Neoproterozoic grains showing a εHf(t) between + 1 and + 14. The deposition age of the Rocha Formation is constrained by the youngest detrital zircon age peak (660 Ma), and the beginning of the deposition of the Sierra de Aguirre Formation (580 Ma). The data indicate common sources with the Marmora Terrane, and it is thus proposed that the Rocha Formation belongs to the Gariep Belt, and it was juxtaposed during the Ediacaran to the DFB."],["dc.description.sponsorship"," Deutscher Akademischer Austauschdienst http://dx.doi.org/10.13039/501100001655"],["dc.description.sponsorship"," FAPESP 501100001807"],["dc.description.sponsorship"," Georg-August-Universität Göttingen 501100003385"],["dc.identifier.doi","10.1007/s00531-022-02230-0"],["dc.identifier.pii","2230"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/113386"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-597"],["dc.relation.eissn","1437-3262"],["dc.relation.issn","1437-3254"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.title","Reassessing the polyphase Neoproterozoic evolution of the Punta del Este Terrane, Dom Feliciano Belt, Uruguay"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","593"],["dc.bibliographiccitation.lastpage","614"],["dc.contributor.author","Oriolo, S."],["dc.contributor.author","Hueck, Mathias"],["dc.contributor.author","Oyhantçabal, P."],["dc.contributor.author","Goscombe, B."],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.contributor.editor","Siegesmund, Siegfried"],["dc.contributor.editor","Oyhantçabal, P."],["dc.contributor.editor","Basei, M. A. S."],["dc.contributor.editor","Oriolo, S."],["dc.date.accessioned","2022-03-07T10:14:16Z"],["dc.date.available","2022-03-07T10:14:16Z"],["dc.date.issued","2018"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/104407"],["dc.publisher","Springer"],["dc.publisher.place","Berlin"],["dc.relation.doi","10.1007/978-3-319-68920-3"],["dc.relation.ispartof","Regional Geology Reviews: Geology of Southwest Gondwans"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Shear zones in Brasiliano–Pan-African Belts and their role in the amalgamation and break-up of southwestern Gondwana"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","324"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Journal of South American Earth Sciences"],["dc.bibliographiccitation.lastpage","350"],["dc.bibliographiccitation.volume","32"],["dc.contributor.author","Basei, Miguel A. S."],["dc.contributor.author","Campos Neto, M. C."],["dc.contributor.author","Castro, Nuno"],["dc.contributor.author","Nutman, A. P."],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Yamamoto, M. T."],["dc.contributor.author","Hueck, Mathias"],["dc.contributor.author","Osako, L."],["dc.contributor.author","Siga, O."],["dc.contributor.author","Passarelli, Chiara"],["dc.date.accessioned","2018-11-07T08:49:13Z"],["dc.date.available","2018-11-07T08:49:13Z"],["dc.date.issued","2011"],["dc.description.abstract","The Dom Feliciano Belt constitutes the main geotectonic unit of the southeastern portion of Brazil and Uruguay. It was formed by the end of the Neoproterozoic as a result of the interaction among the Rio de La Plata, Paranapanema, Congo and Kalahari cratons during the formation of Western Gondwana. The Brusque Group represents the supracrustal units of the Dom Feliciano Belt that occur in its northernmost part, which ends in the Brazilian coast and probable continuity in the Kaoko Belt in southwestern Africa. It is possible to constrain the evolution of the Brusque Group paleobasin to the Neoproterozoic, with the rift phase starting in the Tonian (940-840 Ma) and the main sedimentation occurring until 640 Ma, as indicated by the ages of the acid volcanic rocks intercalated with the metasedimentary sequence. The supracrustal rocks can be grouped in three main units lithostratigraphically organized from the oldest to the youngest: Rio Oliveira Formation (rift phase, predominating metavolcanic units), Botuvera Formation (metasedimentary) and Rio da Areia Formation (metavolcano-carbonatic). Between 640 and 600 Ma several metamorphism and deformation phases affected the Brusque Group. Around 600 +/- 10 Ma the three granitic suites (Sao Joao Batista, Valsungana and Nova Trento) were emplaced within regional metamorphites, producing post-foliation S2 metamorphic aureoles. S2 represents the main foliation observed in the metavolcanosedimentary rocks that constitute the Brusque Group. The tectonic model for the evolution of Brusque Group can be better achieved only when the geochemical, isotopic and geochronologic information available for the Dom Feliciano Belt in Santa Catarina, is considered as a whole. Therefore it is here suggested that the Brusque Group initially evolved in an independent peri-cratonic basin setting separated from the Florianopolis - Pelotas-Aigua magmatic arc by the Adamastor ocean, having been juxtaposed to it only around 600 Ma, when Brusque Group and the Florianopolis Batholith collided. (C) 2011 Elsevier Ltd. All rights reserved."],["dc.identifier.doi","10.1016/j.jsames.2011.03.016"],["dc.identifier.isi","000298464900007"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/21405"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","0895-9811"],["dc.title","Tectonic evolution of the Brusque Group, Dom Feliciano belt, Santa Catarina, Southern Brazil"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","59"],["dc.bibliographiccitation.journal","Journal of Structural Geology"],["dc.bibliographiccitation.lastpage","78"],["dc.bibliographiccitation.volume","92"],["dc.contributor.author","Oriolo, Sebastian"],["dc.contributor.author","Oyhantcabal, Pedro"],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Heidelbach, Florian"],["dc.contributor.author","Pfaender, Joerg A."],["dc.contributor.author","Basei, Miguel A. S."],["dc.contributor.author","Hueck, Mathias"],["dc.contributor.author","Hannich, Felix"],["dc.contributor.author","Sperner, Blanka"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.date.accessioned","2018-11-07T10:06:28Z"],["dc.date.available","2018-11-07T10:06:28Z"],["dc.date.issued","2016"],["dc.description.abstract","New structural, microstructural and geochronological (U-Pb LA-ICP-MS, Ar/Ar, K-Ar, Rb-Sr) data were obtained for the Dom Feliciano Belt in Uruguay. The main phase of crustal shortening, metamorphism and associated exhumation is recorded between 630 and 600 Ma. This stage is related to the collision of the Rio de la Plata and Congo cratons at ca. 630 Ma, which also involved crustal reworking of minor crustal blocks such as the Nico Perez Terrane and voluminous post-collisional magmatism. Subsequent orogen-parallel sinistral shearing gave rise to further deformation up to ca. 584 Ma and resulted from the onset of the convergence of the Kalahari Craton and the Rio de la Plata-Congo cratons. Sinistral shear zones underwent progressive strain localization and retrograde conditions of deformation during crustal exhumation. Dextral ENE-striking shear zones were subsequently active at ca. 550 Ma, coeval with further sinistral shearing along N- to NNE-striking shear zones. The tectonothermal evolution of the Dom Feliciano Belt thus recorded the collision of the Rio de la Plata and Congo cratons, which comprised one of the first amalgamated nuclei of Gondwana, and the subsequent incorporation of the Kalahari Craton into Western Gondwana. (C) 2016 Elsevier Ltd. All rights reserved."],["dc.description.sponsorship","DAAD [A/12/75051]; DFG grant [He3258/2-1]"],["dc.identifier.doi","10.1016/j.jsg.2016.09.010"],["dc.identifier.isi","000387196000005"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/39098"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0191-8141"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Shear zone evolution and timing of deformation in the Neoproterozoic transpressional Dom Feliciano Belt, Uruguay"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","S0895981121004673"],["dc.bibliographiccitation.firstpage","103621"],["dc.bibliographiccitation.journal","Journal of South American Earth Sciences"],["dc.bibliographiccitation.volume","112"],["dc.contributor.author","Oriolo, Sebastián"],["dc.contributor.author","Hueck, Mathias"],["dc.contributor.author","Oyhantçabal, Pedro"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.date.accessioned","2022-02-01T10:32:10Z"],["dc.date.available","2022-02-01T10:32:10Z"],["dc.date.issued","2021"],["dc.identifier.doi","10.1016/j.jsames.2021.103621"],["dc.identifier.pii","S0895981121004673"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/99024"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-517"],["dc.relation.issn","0895-9811"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.rights.uri","https://www.elsevier.com/tdm/userlicense/1.0/"],["dc.title","The Precambrian to Paleozoic crustal growth of South America: From collisional to accretionary tectonics"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","4068"],["dc.bibliographiccitation.issue","10"],["dc.bibliographiccitation.journal","Tectonics"],["dc.bibliographiccitation.lastpage","4085"],["dc.bibliographiccitation.volume","37"],["dc.contributor.author","Hueck, Mathias"],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Heller, Beatrix"],["dc.contributor.author","Stipp Basei, Miguel Angelo"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.date.accessioned","2020-12-10T18:09:23Z"],["dc.date.available","2020-12-10T18:09:23Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1029/2018TC005041"],["dc.identifier.issn","0278-7407"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/73638"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","(U-Th)/He Thermochronology and Zircon Radiation Damage in the South American Passive Margin: Thermal Overprint of the Paraná LIP?"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","593"],["dc.bibliographiccitation.lastpage","613"],["dc.contributor.author","Oriolo, Sebastián"],["dc.contributor.author","Hueck, Mathias"],["dc.contributor.author","Oyhantçabal, Pedro"],["dc.contributor.author","Goscombe, Ben"],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.date.accessioned","2022-03-03T10:28:21Z"],["dc.date.available","2022-03-03T10:28:21Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1007/978-3-319-68920-3_22"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/104312"],["dc.publisher","Springer"],["dc.publisher.place","Cham"],["dc.relation.doi","10.1007/978-3-319-68920-3"],["dc.relation.isbn","978-3-319-68919-7"],["dc.relation.isbn","978-3-319-68920-3"],["dc.relation.ispartof","Geology of Southwest Gondwana"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Shear Zones in Brasiliano-Pan-African Belts and Their Role in the Amalgamation and Break-Up of Southwest Gondwana"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","104199"],["dc.bibliographiccitation.journal","Journal of Structural Geology"],["dc.bibliographiccitation.volume","141"],["dc.contributor.author","Hueck, Mathias"],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Basei, Miguel A.S."],["dc.contributor.author","Philipp, Ruy P."],["dc.contributor.author","Oriolo, Sebastián"],["dc.contributor.author","Heidelbach, Florian"],["dc.contributor.author","Oyhantçabal, Pedro"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.date.accessioned","2021-04-14T08:29:03Z"],["dc.date.available","2021-04-14T08:29:03Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.1016/j.jsg.2020.104199"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/82782"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.relation.issn","0191-8141"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Dating recurrent shear zone activity and the transition from ductile to brittle deformation: White mica geochronology applied to the Neoproterozoic Dom Feliciano Belt in South Brazil"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","609"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Journal of the Geological Society"],["dc.bibliographiccitation.lastpage","626"],["dc.bibliographiccitation.volume","174"],["dc.contributor.author","Hueck, Mathias"],["dc.contributor.author","Oriolo, Sebastian"],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Oyhantcabal, Pedro"],["dc.contributor.author","Schanofski, Max"],["dc.contributor.author","Stipp Basei, Miguel Angelo"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.date.accessioned","2019-07-24T07:26:00Z"],["dc.date.available","2019-07-24T07:26:00Z"],["dc.date.issued","2017"],["dc.description.abstract","The crystalline basement of Uruguay was assembled during the Brasiliano Orogeny in the Neoproterozoic Era and was later affected by discrete tectonic activity. A new multi-method low-temperature dataset including (U–Th)/He ages from both zircon and apatite, T–t modelling and K–Ar dating of fine sericite fractions and fault gouge reveal a detailed post-orogenic geological history spanning the Phanerozoic Eon. The juxtaposition of the terranes that compose the area was achieved in the Ediacaran Period, and post-collision was marked by intense exhumation, in which the crystalline basement reached near-surface conditions by the early to mid-Palaeozoic. Regional subsidence promoted sedimentation in the Paraná Basin until the Permian, covering and reheating much of the basement that is at present exposed. Afterwards, deposition and volcanism were mostly confined to its current limits. Regional exhumation of the shield during the Permo-Triassic exposed much of the northern portion of the basement, and the south was further affected by the opening of the South Atlantic Ocean during the Mesozoic. Little exhumation affected the Uruguayan Shield during the Cenozoic, as reflected in its modest topography. The reactivation of inherited Neoproterozoic structures influenced the development of Mesozoic basins and the present-day landscape. Supplementary material: Supplementary data (sample locations, (U-Th)/He data and K-Ar data) are available at https://doi.org/10.6084/m9.figshare.c.3702043"],["dc.identifier.doi","10.1144/jgs2016-101"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61959"],["dc.language.iso","en"],["dc.relation.issn","0016-7649"],["dc.relation.issn","2041-479X"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Phanerozoic low-temperature evolution of the Uruguayan Shield along the South American passive margin"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","403"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","International Journal of Earth Sciences"],["dc.bibliographiccitation.lastpage","425"],["dc.bibliographiccitation.volume","108"],["dc.contributor.author","Hueck, Mathias"],["dc.contributor.author","Stipp Basei, Miguel Angelo"],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Oriolo, Sebastian"],["dc.contributor.author","Heidelbach, Florian"],["dc.contributor.author","Siegesmund, Siegfried"],["dc.date.accessioned","2019-07-24T07:33:10Z"],["dc.date.available","2019-07-24T07:33:10Z"],["dc.date.issued","2018"],["dc.description.abstract","The Dom Feliciano Belt developed during the Brasiliano–Pan-African orogenic cycle due to the tectonic interaction between the Rio de la Plata, Congo and Kalahari cratons, along with the amalgamation of smaller continental fragments. Together with its prolongations to the south, the Major Gercino Shear Zone constitutes one of the main lineaments of the orogenic system, establishing a more than 1000 km long NE-trending tectonic boundary between a granitic batholith and a metavolcano-sedimentary association. Based on combined field, structural, microstructural and textural data, together with new and published geochronological data, a refined model for the geological evolution of the Major Gercino Shear Zone is presented. Regional NW-verging, low-dipping structures were generated between 650 and 615 Ma, preceding the formation of the shear zone. This was followed by the main deformation phase, corresponding to pure-shear dominated dextral strike-slip, interpreted do be controlled by regional transpression during oblique convergence of the continental terranes. This stage lasted until ca. 585 Ma and was coeval with the continuous emplacement of granitic magmatism along the structure. Strain partitioning and localization led to the development of mylonitic belts along the intrusion borders mostly under greenschist facies metamorphic conditions. Late-stage ductile deformation along the structure was active during the cooling of the intrusions until ca. 550 Ma, while the deformation front of the orogenic system migrated to counterpart orogenic belts in the African continent. After tectonic stabilization, the Major Gercino Shear Zone recorded episodic brittle reactivation, possibly related to the Phanerozoic evolution of the active margins and intracratonic basins in Gondwana."],["dc.identifier.doi","10.1007/s00531-018-1660-4"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61963"],["dc.language.iso","en"],["dc.relation.issn","1437-3254"],["dc.relation.issn","1437-3262"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Evolution of the Major Gercino Shear Zone in the Dom Feliciano Belt, South Brazil, and implications for the assembly of southwestern Gondwana"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]