Matches in SemOpenAlex for { <https://semopenalex.org/work/W2769845641> ?p ?o ?g. }
- W2769845641 endingPage "594" @default.
- W2769845641 startingPage "577" @default.
- W2769845641 abstract "Abstract The Central Asian Orogenic Belt (CAOB) is regarded to have undergone multiple phases of intracontinental deformation during the Meso-Cenozoic. Located in a key position along the southern CAOB, the Alxa Tectonic Belt (ATB) connects the northernmost Tibetan Plateau with the Mongolian Plateau. In this paper we apply apatite U-Pb and fission track thermochronological studies on varieties of samples from the southwestern ATB, in order to constrain its thermal evolution. Precambrian bedrock samples yield late Ordovician-early Silurian (~ 430–450 Ma) and late Permian (~ 257 Ma) apatite U-Pb ages; the late Paleozoic magmatic-sedimentary samples yield relatively consistent early Permian ages from ~ 276 to 290 Ma. These data reveal that the ATB experienced multiple Paleozoic tectono-thermal events, as the samples passed through the apatite U-Pb closure temperature (~ 350–550 °C). We interpret these tectonic events to record the long-lived subduction-accretion processes of the Paleo-Asian Ocean during the formation of the southern CAOB, with possible thermal influence of the Permian Tarim mantle plume. Apatite fission track (AFT) data and thermal history modelling reveal discrete low-temperature thermal events for the ATB, inducing cooling/reheating through the AFT partial annealing zone (~ 120–60 °C). During the Permian, the samples underwent rapid cooling via exhumation or denudation from deep crustal levels to temperatures" @default.
- W2769845641 created "2017-12-04" @default.
- W2769845641 creator A5031810631 @default.
- W2769845641 creator A5046466285 @default.
- W2769845641 creator A5047873001 @default.
- W2769845641 creator A5057911678 @default.
- W2769845641 creator A5060667788 @default.
- W2769845641 creator A5064936522 @default.
- W2769845641 creator A5090122630 @default.
- W2769845641 date "2018-01-01" @default.
- W2769845641 modified "2023-10-18" @default.
- W2769845641 title "Tectono-thermal evolution of the southwestern Alxa Tectonic Belt, NW China: Constrained by apatite U-Pb and fission track thermochronology" @default.
- W2769845641 cites W1667867793 @default.
- W2769845641 cites W1679390913 @default.
- W2769845641 cites W1815706132 @default.
- W2769845641 cites W1883337532 @default.
- W2769845641 cites W1966266712 @default.
- W2769845641 cites W1975821545 @default.
- W2769845641 cites W1994922107 @default.
- W2769845641 cites W1994997277 @default.
- W2769845641 cites W1998028544 @default.
- W2769845641 cites W2000602051 @default.
- W2769845641 cites W2000936451 @default.
- W2769845641 cites W2001847912 @default.
- W2769845641 cites W2002777547 @default.
- W2769845641 cites W2003323528 @default.
- W2769845641 cites W2017720481 @default.
- W2769845641 cites W2027757863 @default.
- W2769845641 cites W2028042452 @default.
- W2769845641 cites W2034428765 @default.
- W2769845641 cites W2035711153 @default.
- W2769845641 cites W2037880887 @default.
- W2769845641 cites W2038907414 @default.
- W2769845641 cites W2051766674 @default.
- W2769845641 cites W2055604456 @default.
- W2769845641 cites W2056335536 @default.
- W2769845641 cites W2057209804 @default.
- W2769845641 cites W2057625526 @default.
- W2769845641 cites W2057639501 @default.
- W2769845641 cites W2059653811 @default.
- W2769845641 cites W2061723916 @default.
- W2769845641 cites W2069883471 @default.
- W2769845641 cites W2070338146 @default.
- W2769845641 cites W2073350342 @default.
- W2769845641 cites W2074493558 @default.
- W2769845641 cites W2077410321 @default.
- W2769845641 cites W2078134024 @default.
- W2769845641 cites W2088988148 @default.
- W2769845641 cites W2089507620 @default.
- W2769845641 cites W2094074034 @default.
- W2769845641 cites W2103651454 @default.
- W2769845641 cites W2105792028 @default.
- W2769845641 cites W2110706788 @default.
- W2769845641 cites W2111144761 @default.
- W2769845641 cites W2114856901 @default.
- W2769845641 cites W2116351028 @default.
- W2769845641 cites W2116875161 @default.
- W2769845641 cites W2130869872 @default.
- W2769845641 cites W213844450 @default.
- W2769845641 cites W2146206140 @default.
- W2769845641 cites W2146384001 @default.
- W2769845641 cites W2162334444 @default.
- W2769845641 cites W2164177215 @default.
- W2769845641 cites W2167799696 @default.
- W2769845641 cites W2190781208 @default.
- W2769845641 cites W2196187836 @default.
- W2769845641 cites W2276992481 @default.
- W2769845641 cites W2342638531 @default.
- W2769845641 cites W2475010014 @default.
- W2769845641 cites W2513494055 @default.
- W2769845641 cites W2567790362 @default.
- W2769845641 cites W2576810156 @default.
- W2769845641 cites W2591645838 @default.
- W2769845641 cites W2612550437 @default.
- W2769845641 cites W2738122598 @default.
- W2769845641 cites W2804688341 @default.
- W2769845641 doi "https://doi.org/10.1016/j.tecto.2017.11.029" @default.
- W2769845641 hasPublicationYear "2018" @default.
- W2769845641 type Work @default.
- W2769845641 sameAs 2769845641 @default.
- W2769845641 citedByCount "27" @default.
- W2769845641 countsByYear W27698456412018 @default.
- W2769845641 countsByYear W27698456412019 @default.
- W2769845641 countsByYear W27698456412020 @default.
- W2769845641 countsByYear W27698456412021 @default.
- W2769845641 countsByYear W27698456412022 @default.
- W2769845641 countsByYear W27698456412023 @default.
- W2769845641 crossrefType "journal-article" @default.
- W2769845641 hasAuthorship W2769845641A5031810631 @default.
- W2769845641 hasAuthorship W2769845641A5046466285 @default.
- W2769845641 hasAuthorship W2769845641A5047873001 @default.
- W2769845641 hasAuthorship W2769845641A5057911678 @default.
- W2769845641 hasAuthorship W2769845641A5060667788 @default.
- W2769845641 hasAuthorship W2769845641A5064936522 @default.
- W2769845641 hasAuthorship W2769845641A5090122630 @default.
- W2769845641 hasConcept C121332964 @default.
- W2769845641 hasConcept C12294094 @default.
- W2769845641 hasConcept C127313418 @default.