FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2345886492> ?p ?o ?g. }

• W2345886492 abstract "Contact aureoles rimming plutonic rocks are the locus of metamorphism and deformations witnessing magma emplacement mechanisms in the crust. In this study, structural and petrological observations are combined to mineral equilibria modelling to unravel the polyphase tectono-metamorphic history of the Permian Sondalo gabbro and its host rock, the Campo unit (Eastern Alps). The Campo unit consists of Grt–St–Ms–Bt–Pl–Qtz ± Sil ± And ± Crd mica schists attesting of a Carboniferous prograde P–T path, reaching 6 kbar/600 °C and subsequently 5.6 kbar/650 °C. This metamorphism is coeval with the formation of a sub-vertical NE–SW trending foliation (S1) and its overprint by a sub-vertical NW–SE trending foliation (S2). The heat brought by the Permian intrusives subsequently caused heating of the Campo unit at around 3–4 kbar/540 °C reflected by regional static crystallization of cordierite and andalusite porphyroblasts. During the intrusion of the Sondalo gabbro, thermal peak conditions are recorded by Grt–Sil–Spl–Crd–Ilm granulitic xenoliths at ~5.5 kbar/930 °C, subsequently exhumed at ~4 kbar during the development of a new foliation (S3). This foliation is localized around the pluton and moderately dips away from the centre of the pluton. In the migmatitic contact aureole, Grt–Sil–Bt–Pl–Qtz–Ilm and Grt–Sil–Crd–Spl–Bt–Kfs–Ilm residual rocks bear the new foliation (S3) and document a decompression from 6 kbar/750 °C to 5 kbar/725 °C and from 5.2 kbar/800 °C to reach 4.8 kbar/770 °C, respectively. The P–T–d paths recorded by the host rock and the xenoliths point to a two-step magma emplacement. First the Sondalo gabbro intruded the Campo unit causing heating of the host rock without deformation at 3–4 kbar. Second, the ductile flow along the pluton margins developed a new foliation (S3) during exhumation of the pluton and its immediate contact aureole from 6 to 4 kbar. Altogether, it indicates a progressive increase in mechanical coupling between the pluton and the host rock during magma emplacement." @default.
• W2345886492 created "2016-06-24" @default.
• W2345886492 creator A5019716051 @default.
• W2345886492 creator A5023033012 @default.
• W2345886492 creator A5053029204 @default.
• W2345886492 creator A5074884425 @default.
• W2345886492 creator A5087656815 @default.
• W2345886492 date "2016-05-01" @default.
• W2345886492 modified "2023-10-09" @default.
• W2345886492 title "The Sondalo gabbro contact aureole (Campo unit, Eastern Alps): implications for mid-crustal mafic magma emplacement" @default.
• W2345886492 cites W1212741249 @default.
• W2345886492 cites W1548147260 @default.
• W2345886492 cites W1564250183 @default.
• W2345886492 cites W1587490095 @default.
• W2345886492 cites W1605368522 @default.
• W2345886492 cites W1830358639 @default.
• W2345886492 cites W1868659645 @default.
• W2345886492 cites W1941197546 @default.
• W2345886492 cites W1967866912 @default.
• W2345886492 cites W1971377743 @default.
• W2345886492 cites W1973012528 @default.
• W2345886492 cites W1981124642 @default.
• W2345886492 cites W1981398171 @default.
• W2345886492 cites W1985160890 @default.
• W2345886492 cites W1988901849 @default.
• W2345886492 cites W1992691425 @default.
• W2345886492 cites W1993321163 @default.
• W2345886492 cites W1995079291 @default.
• W2345886492 cites W1997842666 @default.
• W2345886492 cites W2001150425 @default.
• W2345886492 cites W2005874889 @default.
• W2345886492 cites W2008691821 @default.
• W2345886492 cites W2010124799 @default.
• W2345886492 cites W2016339418 @default.
• W2345886492 cites W2016602232 @default.
• W2345886492 cites W2019375062 @default.
• W2345886492 cites W2022425203 @default.
• W2345886492 cites W2023565929 @default.
• W2345886492 cites W2035045796 @default.
• W2345886492 cites W2037235417 @default.
• W2345886492 cites W2037775252 @default.
• W2345886492 cites W2039039175 @default.
• W2345886492 cites W2040664822 @default.
• W2345886492 cites W2042673680 @default.
• W2345886492 cites W2044188907 @default.
• W2345886492 cites W2045287269 @default.
• W2345886492 cites W2049486454 @default.
• W2345886492 cites W2052045614 @default.
• W2345886492 cites W2052610886 @default.
• W2345886492 cites W2054493155 @default.
• W2345886492 cites W2055459960 @default.
• W2345886492 cites W2056082591 @default.
• W2345886492 cites W2057884798 @default.
• W2345886492 cites W2060622428 @default.
• W2345886492 cites W2062780534 @default.
• W2345886492 cites W2067019494 @default.
• W2345886492 cites W2068144534 @default.
• W2345886492 cites W2068902226 @default.
• W2345886492 cites W2070060377 @default.
• W2345886492 cites W2072877917 @default.
• W2345886492 cites W2074267807 @default.
• W2345886492 cites W2081129468 @default.
• W2345886492 cites W2082148657 @default.
• W2345886492 cites W2086660840 @default.
• W2345886492 cites W2089805636 @default.
• W2345886492 cites W2095449964 @default.
• W2345886492 cites W2107802328 @default.
• W2345886492 cites W2110307237 @default.
• W2345886492 cites W2111774058 @default.
• W2345886492 cites W2120523471 @default.
• W2345886492 cites W2120697819 @default.
• W2345886492 cites W2126440321 @default.
• W2345886492 cites W2126884263 @default.
• W2345886492 cites W2130281340 @default.
• W2345886492 cites W2131360256 @default.
• W2345886492 cites W2136089459 @default.
• W2345886492 cites W2155539674 @default.
• W2345886492 cites W2157404917 @default.
• W2345886492 cites W2165092669 @default.
• W2345886492 cites W2170189319 @default.
• W2345886492 cites W2170802431 @default.
• W2345886492 cites W2316472930 @default.
• W2345886492 cites W2320897138 @default.
• W2345886492 cites W2323291526 @default.
• W2345886492 cites W4211135612 @default.
• W2345886492 cites W98631245 @default.
• W2345886492 doi "https://doi.org/10.1007/s00410-016-1263-7" @default.
• W2345886492 hasPublicationYear "2016" @default.
• W2345886492 type Work @default.
• W2345886492 sameAs 2345886492 @default.
• W2345886492 citedByCount "20" @default.
• W2345886492 countsByYear W23458864922017 @default.
• W2345886492 countsByYear W23458864922018 @default.
• W2345886492 countsByYear W23458864922019 @default.
• W2345886492 countsByYear W23458864922020 @default.
• W2345886492 countsByYear W23458864922021 @default.
• W2345886492 countsByYear W23458864922022 @default.
• W2345886492 countsByYear W23458864922023 @default.
• W2345886492 crossrefType "journal-article" @default.
• W2345886492 hasAuthorship W2345886492A5019716051 @default.

• next