FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1625153604> ?p ?o ?g. }

• W1625153604 endingPage "39" @default.
• W1625153604 startingPage "3" @default.
• W1625153604 abstract "At the transition from the Permian to the Triassic, Eurasia was the site of voluminous flood-basalt extrusion and rifting. Major flood-basalt provinces occur in the Tunguska, Taymyr, Kuznetsk, Verkhoyansk–Vilyuy and Pechora areas, as well as in the South Chinese Emeishen area. Contemporaneous rift systems developed in the West Siberian, South Kara Sea and Pyasina–Khatanga areas, on the Scythian platform and in the West European and Arctic–North Atlantic domain. At the Permo–Triassic transition, major extensional stresses affected apparently Eurasia, and possibly also Pangea, as evidenced by the development of new rift systems. Contemporaneous flood-basalt activity, inducing a global environmental crisis, is interpreted as related to the impingement of major mantle plumes on the base of the Eurasian lithosphere. Moreover, the Permo–Triassic transition coincided with a period of regional uplift and erosion and a low-stand in sea level. Permo–Triassic rifting and mantle plume activity occurred together with a major reorganization of plate boundaries and plate kinematics that marked the transition from the assembly of Pangea to its break-up. This plate reorganization was possibly associated with a reorganization of the global mantle convection system. On the base of the geological record, we recognize short-lived and long-lived plumes with a duration of magmatic activity of some 10–20 million years and 100–150 million years, respectively. The Permo–Triassic Siberian and Emeishan flood-basalt provinces are good examples of “short-lived” plumes, which contrast with such “long lived” plumes as those of Iceland and Hawaii. The global record indicates that mantle plume activity occurred episodically. Purely empirical considerations indicate that times of major mantle plume activity are associated with periods of global mantle convection reorganization during which thermally driven mantle convection is not fully able to facilitate the necessary heat transfer from the core of the Earth to its surface. In this respect, we distinguish between two geodynamically different scenarios for major plume activity. The major Permo–Triassic plume event followed the assembly Pangea and the detachment of deep-seated subduction slabs from the lithosphere. The Early–Middle Cretaceous major plume event, as well as the terminal–Cretaceous–Paleocene plume event, followed a sharp acceleration of global sea-floor spreading rates and the insertion of new subduction zone slabs deep into the mantle. We conclude that global plate kinematics, driven by mantle convection, have a bearing on the development of major mantle plumes and, to a degree, also on the pattern of related flood-basalt magmatism." @default.
• W1625153604 created "2016-06-24" @default.
• W1625153604 creator A5021338684 @default.
• W1625153604 creator A5029383083 @default.
• W1625153604 creator A5034750019 @default.
• W1625153604 creator A5084906149 @default.
• W1625153604 creator A5091837089 @default.
• W1625153604 date "2002-06-01" @default.
• W1625153604 modified "2023-10-17" @default.
• W1625153604 title "Permo–Triassic intraplate magmatism and rifting in Eurasia: implications for mantle plumes and mantle dynamics" @default.
• W1625153604 cites W1588263366 @default.
• W1625153604 cites W1731936587 @default.
• W1625153604 cites W1963643588 @default.
• W1625153604 cites W1966121046 @default.
• W1625153604 cites W1969955164 @default.
• W1625153604 cites W1972274221 @default.
• W1625153604 cites W1973305248 @default.
• W1625153604 cites W1973957871 @default.
• W1625153604 cites W1974589530 @default.
• W1625153604 cites W1976874566 @default.
• W1625153604 cites W1978295352 @default.
• W1625153604 cites W1979682102 @default.
• W1625153604 cites W1983335280 @default.
• W1625153604 cites W1986562513 @default.
• W1625153604 cites W1989809388 @default.
• W1625153604 cites W1991491867 @default.
• W1625153604 cites W1993879966 @default.
• W1625153604 cites W2004091960 @default.
• W1625153604 cites W2004298336 @default.
• W1625153604 cites W2005297899 @default.
• W1625153604 cites W2008978689 @default.
• W1625153604 cites W2013971280 @default.
• W1625153604 cites W2014338623 @default.
• W1625153604 cites W2015638908 @default.
• W1625153604 cites W2015888344 @default.
• W1625153604 cites W2017953040 @default.
• W1625153604 cites W2018396915 @default.
• W1625153604 cites W2019297867 @default.
• W1625153604 cites W2020301204 @default.
• W1625153604 cites W2025634114 @default.
• W1625153604 cites W2025727391 @default.
• W1625153604 cites W2027425485 @default.
• W1625153604 cites W2028032600 @default.
• W1625153604 cites W2029403887 @default.
• W1625153604 cites W2033204481 @default.
• W1625153604 cites W2039982831 @default.
• W1625153604 cites W2040829729 @default.
• W1625153604 cites W2043022340 @default.
• W1625153604 cites W2043114646 @default.
• W1625153604 cites W2044513826 @default.
• W1625153604 cites W2044753344 @default.
• W1625153604 cites W2044967324 @default.
• W1625153604 cites W2046338166 @default.
• W1625153604 cites W2048799244 @default.
• W1625153604 cites W2049885524 @default.
• W1625153604 cites W2051819341 @default.
• W1625153604 cites W2055515139 @default.
• W1625153604 cites W2058884294 @default.
• W1625153604 cites W2059382524 @default.
• W1625153604 cites W2062221814 @default.
• W1625153604 cites W2066300646 @default.
• W1625153604 cites W2067997488 @default.
• W1625153604 cites W2068564701 @default.
• W1625153604 cites W2073440210 @default.
• W1625153604 cites W2074649309 @default.
• W1625153604 cites W2078137341 @default.
• W1625153604 cites W2079477398 @default.
• W1625153604 cites W2079567648 @default.
• W1625153604 cites W2081296107 @default.
• W1625153604 cites W2087447624 @default.
• W1625153604 cites W2088016718 @default.
• W1625153604 cites W2089096123 @default.
• W1625153604 cites W2089334537 @default.
• W1625153604 cites W2089901911 @default.
• W1625153604 cites W2091828485 @default.
• W1625153604 cites W2092041921 @default.
• W1625153604 cites W2094486238 @default.
• W1625153604 cites W2101386673 @default.
• W1625153604 cites W2102037077 @default.
• W1625153604 cites W2104977665 @default.
• W1625153604 cites W2115497827 @default.
• W1625153604 cites W2116955241 @default.
• W1625153604 cites W2120083369 @default.
• W1625153604 cites W2130291743 @default.
• W1625153604 cites W2133518349 @default.
• W1625153604 cites W2143571800 @default.
• W1625153604 cites W2149665349 @default.
• W1625153604 cites W2149834442 @default.
• W1625153604 cites W2153846210 @default.
• W1625153604 cites W2158350227 @default.
• W1625153604 cites W2163555078 @default.
• W1625153604 cites W2164492815 @default.
• W1625153604 cites W4250227819 @default.
• W1625153604 cites W4292198158 @default.
• W1625153604 doi "https://doi.org/10.1016/s0040-1951(02)00123-3" @default.
• W1625153604 hasPublicationYear "2002" @default.
• W1625153604 type Work @default.
• W1625153604 sameAs 1625153604 @default.

• next