FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2018601145> ?p ?o ?g. }

• W2018601145 endingPage "328" @default.
• W2018601145 startingPage "316" @default.
• W2018601145 abstract "Tectonically active Vindhyan intracratonic basin situated in central India, forms one of the largest Proterozoic sedimentary basins of the world. Possibility of hydrocarbon occurrences in thick sediments of the southern part of this basin, has led to surge in geological and geophysical investigations by various agencies. An attempt to synthesize such multiparametric data in an integrated manner, has provided a new understanding to the prevailing crustal configuration, thermal regime and nature of its geodynamic evolution. Apparently, this region has been subjected to sustained uplift, erosion and magmatism followed by crustal extension, rifting and subsidence due to episodic thermal interaction of the crust with the hot underlying mantle. Almost 5–6 km thick sedimentation took place in the deep faulted Jabera Basin, either directly over the Bijawar/Mahakoshal group of mafic rocks or high velocity-high density exhumed middle part of the crust. Detailed gravity observations indicate further extension of the basin probably beyond NSL rift in the south. A high heat flow of about 78 mW/m2 has also been estimated for this basin, which is characterized by extremely high Moho temperatures (exceeding 1000 °C) and mantle heat flow (56 mW/m2) besides a very thin lithospheric lid of only about 50 km. Many areas of this terrain are thickly underplated by infused magmas and from some segments, granitic–gneissic upper crust has either been completely eroded or now only a thin veneer of such rocks exists due to sustained exhumation of deep seated rocks. A 5–8 km thick retrogressed metasomatized zone, with significantly reduced velocities, has also been identified around mid to lower crustal transition." @default.
• W2018601145 created "2016-06-24" @default.
• W2018601145 creator A5001033968 @default.
• W2018601145 creator A5032009839 @default.
• W2018601145 creator A5054798781 @default.
• W2018601145 creator A5071363632 @default.
• W2018601145 creator A5083444237 @default.
• W2018601145 date "2014-09-01" @default.
• W2018601145 modified "2023-10-16" @default.
• W2018601145 title "Anomalous crustal and lithospheric mantle structure of southern part of the Vindhyan Basin and its geodynamic implications" @default.
• W2018601145 cites W1963989533 @default.
• W2018601145 cites W1973921879 @default.
• W2018601145 cites W1975174437 @default.
• W2018601145 cites W1977174688 @default.
• W2018601145 cites W1977203117 @default.
• W2018601145 cites W1977889596 @default.
• W2018601145 cites W1986569651 @default.
• W2018601145 cites W1986738852 @default.
• W2018601145 cites W1988916862 @default.
• W2018601145 cites W2007701111 @default.
• W2018601145 cites W2010084369 @default.
• W2018601145 cites W2012757044 @default.
• W2018601145 cites W2019289902 @default.
• W2018601145 cites W2025841258 @default.
• W2018601145 cites W2028135028 @default.
• W2018601145 cites W2028345553 @default.
• W2018601145 cites W2036626126 @default.
• W2018601145 cites W2047559336 @default.
• W2018601145 cites W2049173580 @default.
• W2018601145 cites W2050783965 @default.
• W2018601145 cites W2051820082 @default.
• W2018601145 cites W2057416838 @default.
• W2018601145 cites W2064506726 @default.
• W2018601145 cites W2066427264 @default.
• W2018601145 cites W2072327306 @default.
• W2018601145 cites W2073157831 @default.
• W2018601145 cites W2073421208 @default.
• W2018601145 cites W2079330326 @default.
• W2018601145 cites W2079914258 @default.
• W2018601145 cites W2082410254 @default.
• W2018601145 cites W2086121230 @default.
• W2018601145 cites W2090325887 @default.
• W2018601145 cites W2092752157 @default.
• W2018601145 cites W2117167376 @default.
• W2018601145 cites W2118944143 @default.
• W2018601145 cites W2121655921 @default.
• W2018601145 cites W2126218823 @default.
• W2018601145 cites W2135559555 @default.
• W2018601145 cites W2140552111 @default.
• W2018601145 cites W2141419570 @default.
• W2018601145 cites W2142937339 @default.
• W2018601145 cites W2159526931 @default.
• W2018601145 cites W2166211061 @default.
• W2018601145 doi "https://doi.org/10.1016/j.jseaes.2013.11.015" @default.
• W2018601145 hasPublicationYear "2014" @default.
• W2018601145 type Work @default.
• W2018601145 sameAs 2018601145 @default.
• W2018601145 citedByCount "13" @default.
• W2018601145 countsByYear W20186011452014 @default.
• W2018601145 countsByYear W20186011452016 @default.
• W2018601145 countsByYear W20186011452018 @default.
• W2018601145 countsByYear W20186011452019 @default.
• W2018601145 countsByYear W20186011452020 @default.
• W2018601145 countsByYear W20186011452022 @default.
• W2018601145 countsByYear W20186011452023 @default.
• W2018601145 crossrefType "journal-article" @default.
• W2018601145 hasAuthorship W2018601145A5001033968 @default.
• W2018601145 hasAuthorship W2018601145A5032009839 @default.
• W2018601145 hasAuthorship W2018601145A5054798781 @default.
• W2018601145 hasAuthorship W2018601145A5071363632 @default.
• W2018601145 hasAuthorship W2018601145A5083444237 @default.
• W2018601145 hasConcept C109007969 @default.
• W2018601145 hasConcept C114793014 @default.
• W2018601145 hasConcept C127313418 @default.
• W2018601145 hasConcept C151730666 @default.
• W2018601145 hasConcept C162973429 @default.
• W2018601145 hasConcept C16942324 @default.
• W2018601145 hasConcept C17409809 @default.
• W2018601145 hasConcept C200646496 @default.
• W2018601145 hasConcept C2776698055 @default.
• W2018601145 hasConcept C50682988 @default.
• W2018601145 hasConcept C5900021 @default.
• W2018601145 hasConcept C6494504 @default.
• W2018601145 hasConcept C67236022 @default.
• W2018601145 hasConcept C77928131 @default.
• W2018601145 hasConcept C8058405 @default.
• W2018601145 hasConcept C97995005 @default.
• W2018601145 hasConceptScore W2018601145C109007969 @default.
• W2018601145 hasConceptScore W2018601145C114793014 @default.
• W2018601145 hasConceptScore W2018601145C127313418 @default.
• W2018601145 hasConceptScore W2018601145C151730666 @default.
• W2018601145 hasConceptScore W2018601145C162973429 @default.
• W2018601145 hasConceptScore W2018601145C16942324 @default.
• W2018601145 hasConceptScore W2018601145C17409809 @default.
• W2018601145 hasConceptScore W2018601145C200646496 @default.
• W2018601145 hasConceptScore W2018601145C2776698055 @default.
• W2018601145 hasConceptScore W2018601145C50682988 @default.
• W2018601145 hasConceptScore W2018601145C5900021 @default.

• next