Matches in SemOpenAlex for { <https://semopenalex.org/work/W4376141657> ?p ?o ?g. }
- W4376141657 endingPage "26" @default.
- W4376141657 startingPage "1" @default.
- W4376141657 abstract "Across western and northern Chukotka, a region spanning 400 000 km2, we have defined three different tectono-magmatic systems that were active during the Aptian-Albian (123–100 Ma) time span: (1) the Tytylveem post-collisional belt (123–105 Ma); (2) the Chaun province of extension-related magmatism (109–100 Ma); and (3) the earliest eruptive units (106–100 Ma) of the subduction-related Okhotsk-Chukotka volcanic belt (OCVB). The observed tectono-magmatic systems are characterized by their location and by their different chemical and isotopic compositions. The general enrichment of magma sources successively increases from the OCVB to the Tytylveem belt and then to the Chaun province. While the Tytylveem belt was active, the volcanic loci shifted northwest along the strike of the belt, perhaps because of diachronous delamination of the lithosphere of the once present, but extinct, South Anyui ocean. On the scale of the entire region of NE Asia, the tectonic re-arrangement that controlled magmatism in the Early Cretaceous was marked by the extinction of major subduction zones on the periphery of the closing Oimyakon and South Anyui oceanic basins followed by magmatic events likely caused by lithospheric delamination and/or extension. Along the Pacific margin of Asia, subduction-related volcanism was nearly continuous during the entire Cretaceous." @default.
- W4376141657 created "2023-05-12" @default.
- W4376141657 creator A5001111193 @default.
- W4376141657 creator A5016281695 @default.
- W4376141657 creator A5016640393 @default.
- W4376141657 creator A5022989698 @default.
- W4376141657 creator A5031338551 @default.
- W4376141657 creator A5048136135 @default.
- W4376141657 creator A5075694475 @default.
- W4376141657 creator A5077261903 @default.
- W4376141657 creator A5080040672 @default.
- W4376141657 creator A5089222305 @default.
- W4376141657 date "2023-05-10" @default.
- W4376141657 modified "2023-09-26" @default.
- W4376141657 title "Evolution of Aptian and Albian magmatism of Western and Northern Chukotka (Northeast Russia) based on zircon U-Pb geochronology and rock geochemistry" @default.
- W4376141657 cites W1764818718 @default.
- W4376141657 cites W1967248360 @default.
- W4376141657 cites W1969834866 @default.
- W4376141657 cites W1976876082 @default.
- W4376141657 cites W1978640446 @default.
- W4376141657 cites W1980413370 @default.
- W4376141657 cites W1987501517 @default.
- W4376141657 cites W1996768357 @default.
- W4376141657 cites W2007914104 @default.
- W4376141657 cites W2010161889 @default.
- W4376141657 cites W2010186865 @default.
- W4376141657 cites W2016018815 @default.
- W4376141657 cites W2028373945 @default.
- W4376141657 cites W2047383053 @default.
- W4376141657 cites W2048857036 @default.
- W4376141657 cites W2052384428 @default.
- W4376141657 cites W2053070858 @default.
- W4376141657 cites W2055374055 @default.
- W4376141657 cites W2056423071 @default.
- W4376141657 cites W2057785858 @default.
- W4376141657 cites W2062854773 @default.
- W4376141657 cites W2065016109 @default.
- W4376141657 cites W2068659572 @default.
- W4376141657 cites W2075644008 @default.
- W4376141657 cites W2080487384 @default.
- W4376141657 cites W2083286618 @default.
- W4376141657 cites W2089643373 @default.
- W4376141657 cites W2107725925 @default.
- W4376141657 cites W2110829756 @default.
- W4376141657 cites W2111129265 @default.
- W4376141657 cites W2115322124 @default.
- W4376141657 cites W2138522501 @default.
- W4376141657 cites W2144222955 @default.
- W4376141657 cites W2254863569 @default.
- W4376141657 cites W2332667845 @default.
- W4376141657 cites W2466875164 @default.
- W4376141657 cites W2495601659 @default.
- W4376141657 cites W2515405574 @default.
- W4376141657 cites W2606675297 @default.
- W4376141657 cites W2736039065 @default.
- W4376141657 cites W2753035275 @default.
- W4376141657 cites W2897765436 @default.
- W4376141657 cites W2911974429 @default.
- W4376141657 cites W2934555391 @default.
- W4376141657 cites W2939685857 @default.
- W4376141657 cites W2950251225 @default.
- W4376141657 cites W2959013771 @default.
- W4376141657 cites W2983864707 @default.
- W4376141657 cites W2993213520 @default.
- W4376141657 cites W3000000575 @default.
- W4376141657 cites W3011180108 @default.
- W4376141657 cites W3017036477 @default.
- W4376141657 cites W3042961704 @default.
- W4376141657 cites W3047318783 @default.
- W4376141657 cites W3118973340 @default.
- W4376141657 cites W3122452601 @default.
- W4376141657 cites W3134053263 @default.
- W4376141657 cites W3138916328 @default.
- W4376141657 cites W3158558117 @default.
- W4376141657 cites W3185632660 @default.
- W4376141657 cites W3195481652 @default.
- W4376141657 cites W3217234029 @default.
- W4376141657 cites W3217499841 @default.
- W4376141657 cites W4205749704 @default.
- W4376141657 cites W4210666682 @default.
- W4376141657 cites W4229031791 @default.
- W4376141657 cites W4285221394 @default.
- W4376141657 cites W912669999 @default.
- W4376141657 cites W989633556 @default.
- W4376141657 cites W2610817023 @default.
- W4376141657 cites W2618707037 @default.
- W4376141657 doi "https://doi.org/10.1080/00206814.2023.2205494" @default.
- W4376141657 hasPublicationYear "2023" @default.
- W4376141657 type Work @default.
- W4376141657 citedByCount "0" @default.
- W4376141657 crossrefType "journal-article" @default.
- W4376141657 hasAuthorship W4376141657A5001111193 @default.
- W4376141657 hasAuthorship W4376141657A5016281695 @default.
- W4376141657 hasAuthorship W4376141657A5016640393 @default.
- W4376141657 hasAuthorship W4376141657A5022989698 @default.
- W4376141657 hasAuthorship W4376141657A5031338551 @default.
- W4376141657 hasAuthorship W4376141657A5048136135 @default.
- W4376141657 hasAuthorship W4376141657A5075694475 @default.