FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2015288718> ?p ?o ?g. }

• W2015288718 endingPage "281" @default.
• W2015288718 startingPage "269" @default.
• W2015288718 abstract "The main petroliferous basins in eastern China are Cenozoic fault basins, most of which have experienced two-stage tectonic evolution, i.e., rifting subsidence in the Paleogene and post-rifting thermal subsidence in the Neogene-Quaternary. The episodic tectonic evolution and syndepositional faulting had significant influence on the fault basins in terms of accommodation space, deposition rate, and depositional facies zones. In this study, the tectonic deformation characteristics and the tectonic-depositional evolution of the Western Sag of the Cenozoic Liaohe Depression were investigated by comprehensive analysis of the available geological and geophysical data using the modern theory of tectonic geology and the balanced section technique. The tectonic deformation of the Cenozoic fault basin was characterized by superimposed faults and depression. In addition, there existed relatively independent but still related extensional tectonic systems and strike-slip tectonic systems. The tectonic evolution of the fault basin involved five stages, i.e., initial rifting stage (E2s4), intense faulting stage (E2s3), fault-depression transition stage (E3s1–2), differential uplifting stage (E3d), and depression stage (N-Q). According to the characteristics of tectonic development and evolution of the Western Sag, the depositional evolution in the Cenozoic fault basin was divided into two stages, i.e., multi-episodic rifting filling in the Paleogene and post-rifting filling in the Neogene-Quaternary. The former rifting stage was further subdivided into four episodes with different characteristics of depositional development. The episodic faulting controlled the filling process and filling pattern of the Cenozoic Western Sag as well as the development and spatial distribution of associated depositional systems, whereas the syndepositional faults that developed in multiple stages in various tectonic positions controlled the development of depositional systems and sand bodies in the Western Sag. That is, the fault terraces on steep slopes controlled the development of sand bodies, the fault terraces on gentle slopes controlled the development of low-stand fan bodies, and the fault terraces or fault troughs in the central basin controlled the development of fluxoturbidite bodies." @default.
• W2015288718 created "2016-06-24" @default.
• W2015288718 creator A5002711718 @default.
• W2015288718 creator A5031257701 @default.
• W2015288718 creator A5045494817 @default.
• W2015288718 creator A5062707438 @default.
• W2015288718 creator A5074039774 @default.
• W2015288718 date "2013-08-14" @default.
• W2015288718 modified "2023-10-06" @default.
• W2015288718 title "Tectonic evolution and its control over deposition in fault basins: A case study of the Western Sag of the Cenozoic Liaohe Depression, eastern China" @default.
• W2015288718 cites W1953807521 @default.
• W2015288718 cites W1967107641 @default.
• W2015288718 cites W1971550781 @default.
• W2015288718 cites W1972294502 @default.
• W2015288718 cites W1985702115 @default.
• W2015288718 cites W2001377573 @default.
• W2015288718 cites W2006443828 @default.
• W2015288718 cites W2008132927 @default.
• W2015288718 cites W2028244121 @default.
• W2015288718 cites W2033901994 @default.
• W2015288718 cites W2036040703 @default.
• W2015288718 cites W2046816255 @default.
• W2015288718 cites W2063635897 @default.
• W2015288718 cites W2069685514 @default.
• W2015288718 cites W2078311111 @default.
• W2015288718 cites W2094740266 @default.
• W2015288718 cites W2098116826 @default.
• W2015288718 cites W2106228210 @default.
• W2015288718 cites W2106802871 @default.
• W2015288718 cites W2127162022 @default.
• W2015288718 cites W2139852070 @default.
• W2015288718 cites W2150541755 @default.
• W2015288718 cites W2171024874 @default.
• W2015288718 cites W2320397274 @default.
• W2015288718 cites W2338150400 @default.
• W2015288718 cites W4235792179 @default.
• W2015288718 cites W4249581307 @default.
• W2015288718 cites W4254922999 @default.
• W2015288718 cites W2315357886 @default.
• W2015288718 doi "https://doi.org/10.1007/s12182-013-0276-3" @default.
• W2015288718 hasPublicationYear "2013" @default.
• W2015288718 type Work @default.
• W2015288718 sameAs 2015288718 @default.
• W2015288718 citedByCount "5" @default.
• W2015288718 countsByYear W20152887182015 @default.
• W2015288718 countsByYear W20152887182016 @default.
• W2015288718 countsByYear W20152887182017 @default.
• W2015288718 countsByYear W20152887182023 @default.
• W2015288718 crossrefType "journal-article" @default.
• W2015288718 hasAuthorship W2015288718A5002711718 @default.
• W2015288718 hasAuthorship W2015288718A5031257701 @default.
• W2015288718 hasAuthorship W2015288718A5045494817 @default.
• W2015288718 hasAuthorship W2015288718A5062707438 @default.
• W2015288718 hasAuthorship W2015288718A5074039774 @default.
• W2015288718 hasBestOaLocation W20152887181 @default.
• W2015288718 hasConcept C100951216 @default.
• W2015288718 hasConcept C109007969 @default.
• W2015288718 hasConcept C126753816 @default.
• W2015288718 hasConcept C127313418 @default.
• W2015288718 hasConcept C151730666 @default.
• W2015288718 hasConcept C169162353 @default.
• W2015288718 hasConcept C175551986 @default.
• W2015288718 hasConcept C204330871 @default.
• W2015288718 hasConcept C25980409 @default.
• W2015288718 hasConcept C27492601 @default.
• W2015288718 hasConcept C50682988 @default.
• W2015288718 hasConcept C73707237 @default.
• W2015288718 hasConcept C77928131 @default.
• W2015288718 hasConceptScore W2015288718C100951216 @default.
• W2015288718 hasConceptScore W2015288718C109007969 @default.
• W2015288718 hasConceptScore W2015288718C126753816 @default.
• W2015288718 hasConceptScore W2015288718C127313418 @default.
• W2015288718 hasConceptScore W2015288718C151730666 @default.
• W2015288718 hasConceptScore W2015288718C169162353 @default.
• W2015288718 hasConceptScore W2015288718C175551986 @default.
• W2015288718 hasConceptScore W2015288718C204330871 @default.
• W2015288718 hasConceptScore W2015288718C25980409 @default.
• W2015288718 hasConceptScore W2015288718C27492601 @default.
• W2015288718 hasConceptScore W2015288718C50682988 @default.
• W2015288718 hasConceptScore W2015288718C73707237 @default.
• W2015288718 hasConceptScore W2015288718C77928131 @default.
• W2015288718 hasIssue "3" @default.
• W2015288718 hasLocation W20152887181 @default.
• W2015288718 hasOpenAccess W2015288718 @default.
• W2015288718 hasPrimaryLocation W20152887181 @default.
• W2015288718 hasRelatedWork W1993844322 @default.
• W2015288718 hasRelatedWork W2058504808 @default.
• W2015288718 hasRelatedWork W2072757534 @default.
• W2015288718 hasRelatedWork W2316734356 @default.
• W2015288718 hasRelatedWork W2359445152 @default.
• W2015288718 hasRelatedWork W2362159398 @default.
• W2015288718 hasRelatedWork W2367059172 @default.
• W2015288718 hasRelatedWork W2392796846 @default.
• W2015288718 hasRelatedWork W2907799857 @default.
• W2015288718 hasRelatedWork W4386770771 @default.
• W2015288718 hasVolume "10" @default.
• W2015288718 isParatext "false" @default.
• W2015288718 isRetracted "false" @default.

• next