FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2029988187> ?p ?o ?g. }

• W2029988187 endingPage "257" @default.
• W2029988187 startingPage "244" @default.
• W2029988187 abstract "The Qinling Orogen was formed from the closure of the northernmost paleo-Tethys sea and the tectonic suturing of the Yangtze and North China Cratons. The timing of this collision and the tectonic framework are debated. The widely developed Triassic granitoids in the western Qinling Orogen offer a key to understand the tectonic evolution of this region. Here we compile the geological, geochemical and geochronological data of the Triassic granitoids from the Qingling Orogen and conclude that the granitoids north of the Mian-Lue Suture were emplaced in an active continental margin related to the northward subduction of the Mian-Lue oceanic plate during 248 − 200 Ma. The granitoids can be classified into I- and S-types, with the former constituting the major variety. Northward from the Mian-Lue Fault, an S-type granite belt appears, followed by and locally overlapping with an I-type granite belt. The I-type granite belt can be subdivided into four sub-belts from south to north, with increasing contents of K2O, K2O + Na2O, SiO2, Th and U, and the ratios of K2O/Na2O, Rb/Sr and (87Sr/86Sr)i, but decreasing contents of Na2O, Al2O3, Mg#, and εHf(t), except for the northernmost belt which occurs in the Huaxiong Block of the North China Craton. This geochemical polarity of I-type granitoids and the zoned distribution of S- and I-types granitoids cannot be explained through continental collision orogeny (including syn- to post-collision), but can be well interpreted by considering the progressive subduction of the northernmost branch of the paleo-Tethys, as represented by the Mian-Lue Ocean. Thus, the termination of the northernmost paleo-Tethys and the onset of the continental collision between the Yangtze and the North China plates are considered to have occurred at about 200 Ma, during the transition from Triassic to Jurassic. Our model is also supported by the available data from other studies and provides a revised framework for the timing and tectonics of assembly of the Yangtze and the North China Cratons." @default.
• W2029988187 created "2016-06-24" @default.
• W2029988187 creator A5036142816 @default.
• W2029988187 creator A5037985249 @default.
• W2029988187 creator A5048842584 @default.
• W2029988187 creator A5060053337 @default.
• W2029988187 date "2015-01-01" @default.
• W2029988187 modified "2023-10-16" @default.
• W2029988187 title "Compositional polarity of Triassic granitoids in the Qinling Orogen, China: Implication for termination of the northernmost paleo-Tethys" @default.
• W2029988187 cites W1509458422 @default.
• W2029988187 cites W1607995573 @default.
• W2029988187 cites W1871734886 @default.
• W2029988187 cites W1965826523 @default.
• W2029988187 cites W1972591794 @default.
• W2029988187 cites W1972775900 @default.
• W2029988187 cites W1973125903 @default.
• W2029988187 cites W1973506361 @default.
• W2029988187 cites W1974080280 @default.
• W2029988187 cites W1976979379 @default.
• W2029988187 cites W1982070838 @default.
• W2029988187 cites W1982566420 @default.
• W2029988187 cites W1985447869 @default.
• W2029988187 cites W1992924010 @default.
• W2029988187 cites W1993300192 @default.
• W2029988187 cites W1997774186 @default.
• W2029988187 cites W2002463493 @default.
• W2029988187 cites W2003311821 @default.
• W2029988187 cites W2003454252 @default.
• W2029988187 cites W2005078833 @default.
• W2029988187 cites W2007339247 @default.
• W2029988187 cites W2008457037 @default.
• W2029988187 cites W2008693928 @default.
• W2029988187 cites W2012573334 @default.
• W2029988187 cites W2013694956 @default.
• W2029988187 cites W2015063639 @default.
• W2029988187 cites W2016426836 @default.
• W2029988187 cites W2019115661 @default.
• W2029988187 cites W2020304604 @default.
• W2029988187 cites W2020688605 @default.
• W2029988187 cites W2022204890 @default.
• W2029988187 cites W2022896618 @default.
• W2029988187 cites W2024248666 @default.
• W2029988187 cites W2027316964 @default.
• W2029988187 cites W2028642961 @default.
• W2029988187 cites W2029634189 @default.
• W2029988187 cites W2031423471 @default.
• W2029988187 cites W2035422468 @default.
• W2029988187 cites W2037341487 @default.
• W2029988187 cites W2037923466 @default.
• W2029988187 cites W2040730825 @default.
• W2029988187 cites W2041665896 @default.
• W2029988187 cites W2041894015 @default.
• W2029988187 cites W2041989597 @default.
• W2029988187 cites W2044853578 @default.
• W2029988187 cites W2046672205 @default.
• W2029988187 cites W2053162423 @default.
• W2029988187 cites W2053422899 @default.
• W2029988187 cites W2055799747 @default.
• W2029988187 cites W2058370715 @default.
• W2029988187 cites W2060003735 @default.
• W2029988187 cites W2060013614 @default.
• W2029988187 cites W2061189874 @default.
• W2029988187 cites W2063754919 @default.
• W2029988187 cites W2066581757 @default.
• W2029988187 cites W2068745492 @default.
• W2029988187 cites W2076373269 @default.
• W2029988187 cites W2076566162 @default.
• W2029988187 cites W2077414735 @default.
• W2029988187 cites W2078105240 @default.
• W2029988187 cites W2082951334 @default.
• W2029988187 cites W2085217600 @default.
• W2029988187 cites W2088173292 @default.
• W2029988187 cites W2090206242 @default.
• W2029988187 cites W2090282827 @default.
• W2029988187 cites W2092386709 @default.
• W2029988187 cites W2114308984 @default.
• W2029988187 cites W2127517677 @default.
• W2029988187 cites W2130082946 @default.
• W2029988187 cites W2132513592 @default.
• W2029988187 cites W2144172427 @default.
• W2029988187 cites W2145087726 @default.
• W2029988187 cites W2145604970 @default.
• W2029988187 cites W2152275597 @default.
• W2029988187 cites W2153589155 @default.
• W2029988187 cites W2159104880 @default.
• W2029988187 cites W3152098114 @default.
• W2029988187 doi "https://doi.org/10.1016/j.gr.2013.09.017" @default.
• W2029988187 hasPublicationYear "2015" @default.
• W2029988187 type Work @default.
• W2029988187 sameAs 2029988187 @default.
• W2029988187 citedByCount "192" @default.
• W2029988187 countsByYear W20299881872013 @default.
• W2029988187 countsByYear W20299881872014 @default.
• W2029988187 countsByYear W20299881872015 @default.
• W2029988187 countsByYear W20299881872016 @default.
• W2029988187 countsByYear W20299881872017 @default.
• W2029988187 countsByYear W20299881872018 @default.
• W2029988187 countsByYear W20299881872019 @default.

• next