FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4384156733> ?p ?o ?g. }

• W4384156733 endingPage "107285" @default.
• W4384156733 startingPage "107285" @default.
• W4384156733 abstract "The Pamir–Karakoram terrain contains abundant Cretaceous granitoids, and minor coeval volcanic rocks and mafic intrusions, which represent a wide (ca. 400 km) continental arc developed during northward subduction of Neo-Tethys oceanic lithosphere. However, little is known of the tectonic controls on the magmatic flare-ups and their implications for crustal thickening. In this paper, we report new zircon UPb age and Hf isotope data for Cretaceous biotite granites, two-mica granites and mafic microgranular enclaves (MMEs) from the large-scale granitic batholiths in Pamir. These and previously published results show there were four episodes of Cretaceous magmatism (124–108, 107–103, 102–92, and 80–70 Ma). The Cretaceous arc migrated progressively landward from Karakoram to Central Pamir with a maximum arc–trench distance of ca. 400 km during the first magmatic episode (124–108 Ma). The igneous rocks are mainly S-type granites with enriched zircon Hf isotopic compositions (ɛHf(t) = −19.8 to −5.4), indicating derivation by partial melting of metasedimentary units. A magmatic flare-up at 105 ± 2 Ma generated voluminous I-type granites and minor mafic igneous rocks that cover ca. 30% of the study area. The I-type granites have higher zircon ɛHf(t) values (−19.0 to −2.0) as compared with those of the earlier S-type granites, which reflect the addition of mantle-derived materials (ca. 30%). The third episode of magmatism (102–92 Ma) generated mainly intermediate–silicic volcanic rocks, which are geochemically similar to I-type granites and have ɛHf(t) values of −15.0 to −1.5. The final episode of magmatism (80–70 Ma) was dominated by alkaline and mafic igneous rocks formed in a post-collisional setting, which have variable ɛHf(t) values of −6.6 to 10.5. Our study highlights that the Early Cretaceous magmatic flare-up in the Pamir–Karakoram terrain was related to foundering of the flat-slab of Neo-Tethys oceanic lithosphere that was previously subducted, which induced voluminous underplating of mantle-derived magma in the lower crust. This process had a key role in crustal thickening in the Pamir–Karakoram terrain prior to the Cenozoic India–Asia collision." @default.
• W4384156733 created "2023-07-14" @default.
• W4384156733 creator A5000159619 @default.
• W4384156733 creator A5010206164 @default.
• W4384156733 creator A5021645045 @default.
• W4384156733 creator A5028946363 @default.
• W4384156733 creator A5030863883 @default.
• W4384156733 creator A5070296642 @default.
• W4384156733 creator A5073146335 @default.
• W4384156733 creator A5088061918 @default.
• W4384156733 date "2023-10-01" @default.
• W4384156733 modified "2023-10-16" @default.
• W4384156733 title "Cretaceous magmatic migration and flare-up in Pamir–Karakoram" @default.
• W4384156733 cites W1531949059 @default.
• W4384156733 cites W1636091909 @default.
• W4384156733 cites W1828329906 @default.
• W4384156733 cites W1965754569 @default.
• W4384156733 cites W1968247674 @default.
• W4384156733 cites W1969859799 @default.
• W4384156733 cites W1976164114 @default.
• W4384156733 cites W1993581236 @default.
• W4384156733 cites W1994048706 @default.
• W4384156733 cites W2002225417 @default.
• W4384156733 cites W2003954276 @default.
• W4384156733 cites W2004993774 @default.
• W4384156733 cites W2023796783 @default.
• W4384156733 cites W2034091664 @default.
• W4384156733 cites W2036235050 @default.
• W4384156733 cites W2051945738 @default.
• W4384156733 cites W2052079943 @default.
• W4384156733 cites W2071156335 @default.
• W4384156733 cites W2082002326 @default.
• W4384156733 cites W2090446100 @default.
• W4384156733 cites W2100376263 @default.
• W4384156733 cites W2102828314 @default.
• W4384156733 cites W2110464369 @default.
• W4384156733 cites W2119606789 @default.
• W4384156733 cites W2120824396 @default.
• W4384156733 cites W2124698750 @default.
• W4384156733 cites W2128624170 @default.
• W4384156733 cites W2129866727 @default.
• W4384156733 cites W2137027700 @default.
• W4384156733 cites W2156954089 @default.
• W4384156733 cites W2157365719 @default.
• W4384156733 cites W2165982417 @default.
• W4384156733 cites W2169766597 @default.
• W4384156733 cites W2192132413 @default.
• W4384156733 cites W2205343350 @default.
• W4384156733 cites W2274475702 @default.
• W4384156733 cites W2313755883 @default.
• W4384156733 cites W2324678581 @default.
• W4384156733 cites W2327938147 @default.
• W4384156733 cites W2424453843 @default.
• W4384156733 cites W2736435839 @default.
• W4384156733 cites W2744818372 @default.
• W4384156733 cites W2770847974 @default.
• W4384156733 cites W2800500947 @default.
• W4384156733 cites W2810407556 @default.
• W4384156733 cites W2887535355 @default.
• W4384156733 cites W2900851192 @default.
• W4384156733 cites W2905413347 @default.
• W4384156733 cites W2946564934 @default.
• W4384156733 cites W2974955689 @default.
• W4384156733 cites W2991310459 @default.
• W4384156733 cites W2999357645 @default.
• W4384156733 cites W3005816334 @default.
• W4384156733 cites W3008658883 @default.
• W4384156733 cites W3009608873 @default.
• W4384156733 cites W3119208621 @default.
• W4384156733 cites W3160126885 @default.
• W4384156733 cites W3181615550 @default.
• W4384156733 cites W3208082614 @default.
• W4384156733 cites W4210926899 @default.
• W4384156733 cites W4280495615 @default.
• W4384156733 cites W4298137129 @default.
• W4384156733 doi "https://doi.org/10.1016/j.lithos.2023.107285" @default.
• W4384156733 hasPublicationYear "2023" @default.
• W4384156733 type Work @default.
• W4384156733 citedByCount "0" @default.
• W4384156733 crossrefType "journal-article" @default.
• W4384156733 hasAuthorship W4384156733A5000159619 @default.
• W4384156733 hasAuthorship W4384156733A5010206164 @default.
• W4384156733 hasAuthorship W4384156733A5021645045 @default.
• W4384156733 hasAuthorship W4384156733A5028946363 @default.
• W4384156733 hasAuthorship W4384156733A5030863883 @default.
• W4384156733 hasAuthorship W4384156733A5070296642 @default.
• W4384156733 hasAuthorship W4384156733A5073146335 @default.
• W4384156733 hasAuthorship W4384156733A5088061918 @default.
• W4384156733 hasConcept C104962623 @default.
• W4384156733 hasConcept C120806208 @default.
• W4384156733 hasConcept C127313418 @default.
• W4384156733 hasConcept C151730666 @default.
• W4384156733 hasConcept C162973429 @default.
• W4384156733 hasConcept C167284885 @default.
• W4384156733 hasConcept C172660882 @default.
• W4384156733 hasConcept C17409809 @default.
• W4384156733 hasConcept C192241223 @default.
• W4384156733 hasConcept C2777212541 @default.

• next