FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W987984503> ?p ?o ?g. }

• W987984503 endingPage "427" @default.
• W987984503 startingPage "414" @default.
• W987984503 abstract "Destruction of the North China Craton (NCC) in the Mesozoic due to subduction of the Paleo-Pacific Plate has attracted a lot of recent interest, with numerous studies focusing on regional tectonics and associated magmatism. Although the peak ages for this event have been established, the timing of its initiation remains poorly understood. In this paper, two rift basins in the northern Hebei Province of China, the Diaoe Basin (DB) and Houcheng Basin (HB), are studied in order to constrain the timing of destruction of the northern margin of the NCC. Both NNE-striking basins developed on Proterozoic basement. The DB is a graben controlled by normal faults on its two margins, and the HB is a half-graben bounded by normal faults on its eastern side. Basin fills include detrital sediments and volcanic rocks, which are (from bottom to top) the Houcheng Formation (Fh), the Zhangjiakou Formation (Fzh), the Shijiayao Formation (Fs), and the Huajiying Formation (Fhj). The Fh is composed mainly of detrital sediments interlayered with andesite in its lower section, and interlayered with felsic volcanics (rhyolite) in its upper section. There exists a transitional change from the Fh to the thick felsic volcanic strata of the Fzh. Geochemically, the andesite layers in the lower Fh were most likely derived from mixing of crust and mantle melts, whereas the felsic rocks were derived from melting of the lower crust. U–Pb dating of zircons by LA-ICP-MS yielded ages for the lower Fh andesites of ca. 165.7 Ma in the HB and ca. 157.4 Ma in the DB. The felsic rocks at the base of the Fzh yielded ages of ca. 155.1 Ma in the HB and ca. 149.2–143.4 Ma in the DB. The Fs and Fhj in the DB both yielded similar ages of ca. 136 Ma. The development of rift basins, together with the occurrence of massive felsic volcanic rocks, indicates a period of significant extension and thinning of the NCC. The ca. 165.7–155.1 Ma age for andesites not only represents the initial timing of crustal extension, but also the timing of thermally induced melting of the lower lithosphere. We conclude, therefore, that the destruction of the northern margin of the NCC started by the Middle Jurassic or earlier." @default.
• W987984503 created "2016-06-24" @default.
• W987984503 creator A5052350348 @default.
• W987984503 creator A5053370317 @default.
• W987984503 creator A5082091969 @default.
• W987984503 date "2015-11-01" @default.
• W987984503 modified "2023-09-30" @default.
• W987984503 title "Mesozoic tectonic setting of rift basins in eastern North China and implications for destruction of the North China Craton" @default.
• W987984503 cites W1587624588 @default.
• W987984503 cites W1587780337 @default.
• W987984503 cites W1965360760 @default.
• W987984503 cites W1970458022 @default.
• W987984503 cites W1979705656 @default.
• W987984503 cites W1980640006 @default.
• W987984503 cites W1980951510 @default.
• W987984503 cites W1997705537 @default.
• W987984503 cites W2000795509 @default.
• W987984503 cites W2013857416 @default.
• W987984503 cites W2019034794 @default.
• W987984503 cites W2019273078 @default.
• W987984503 cites W2019621021 @default.
• W987984503 cites W2020282576 @default.
• W987984503 cites W2021704348 @default.
• W987984503 cites W2021745934 @default.
• W987984503 cites W2022859730 @default.
• W987984503 cites W2024364472 @default.
• W987984503 cites W2035003573 @default.
• W987984503 cites W2035313346 @default.
• W987984503 cites W2041479996 @default.
• W987984503 cites W2042477030 @default.
• W987984503 cites W2043003723 @default.
• W987984503 cites W2044698216 @default.
• W987984503 cites W2046653975 @default.
• W987984503 cites W2049907150 @default.
• W987984503 cites W2053734248 @default.
• W987984503 cites W2057266647 @default.
• W987984503 cites W2062306363 @default.
• W987984503 cites W2065463075 @default.
• W987984503 cites W2075072653 @default.
• W987984503 cites W2077080626 @default.
• W987984503 cites W2080536253 @default.
• W987984503 cites W2091646615 @default.
• W987984503 cites W2093411929 @default.
• W987984503 cites W2093898661 @default.
• W987984503 cites W2094090764 @default.
• W987984503 cites W2094279761 @default.
• W987984503 cites W2099830405 @default.
• W987984503 cites W2105992741 @default.
• W987984503 cites W2106814179 @default.
• W987984503 cites W2121773243 @default.
• W987984503 cites W2123985829 @default.
• W987984503 cites W2127559886 @default.
• W987984503 cites W2129379483 @default.
• W987984503 cites W2130869872 @default.
• W987984503 cites W2148903621 @default.
• W987984503 cites W2167856052 @default.
• W987984503 cites W2167893737 @default.
• W987984503 cites W2172153902 @default.
• W987984503 cites W2316514264 @default.
• W987984503 cites W2325514473 @default.
• W987984503 doi "https://doi.org/10.1016/j.jseaes.2015.06.022" @default.
• W987984503 hasPublicationYear "2015" @default.
• W987984503 type Work @default.
• W987984503 sameAs 987984503 @default.
• W987984503 citedByCount "29" @default.
• W987984503 countsByYear W9879845032016 @default.
• W987984503 countsByYear W9879845032017 @default.
• W987984503 countsByYear W9879845032018 @default.
• W987984503 countsByYear W9879845032019 @default.
• W987984503 countsByYear W9879845032020 @default.
• W987984503 countsByYear W9879845032021 @default.
• W987984503 countsByYear W9879845032022 @default.
• W987984503 countsByYear W9879845032023 @default.
• W987984503 crossrefType "journal-article" @default.
• W987984503 hasAuthorship W987984503A5052350348 @default.
• W987984503 hasAuthorship W987984503A5053370317 @default.
• W987984503 hasAuthorship W987984503A5082091969 @default.
• W987984503 hasConcept C120806208 @default.
• W987984503 hasConcept C127313418 @default.
• W987984503 hasConcept C147717901 @default.
• W987984503 hasConcept C151730666 @default.
• W987984503 hasConcept C17409809 @default.
• W987984503 hasConcept C192241223 @default.
• W987984503 hasConcept C193429443 @default.
• W987984503 hasConcept C25822816 @default.
• W987984503 hasConcept C2779321686 @default.
• W987984503 hasConcept C36986328 @default.
• W987984503 hasConcept C50682988 @default.
• W987984503 hasConcept C77928131 @default.
• W987984503 hasConceptScore W987984503C120806208 @default.
• W987984503 hasConceptScore W987984503C127313418 @default.
• W987984503 hasConceptScore W987984503C147717901 @default.
• W987984503 hasConceptScore W987984503C151730666 @default.
• W987984503 hasConceptScore W987984503C17409809 @default.
• W987984503 hasConceptScore W987984503C192241223 @default.
• W987984503 hasConceptScore W987984503C193429443 @default.
• W987984503 hasConceptScore W987984503C25822816 @default.
• W987984503 hasConceptScore W987984503C2779321686 @default.

• next