FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2566385010> ?p ?o ?g. }

• W2566385010 endingPage "999" @default.
• W2566385010 startingPage "988" @default.
• W2566385010 abstract "Based on outcrops of the whole basin, drilling and seismic data, this paper makes a systematic analysis of Neoproterozoic basin stratigraphic distribution and tectonic evolution characteristics in Tarim. Under the control of the aggregation and breakup of Rodinia supercontinent, the extensional sedimentary basin formed with North-South differences in the Neoproterozoic, separated by the middle ancient land. There is a sedimentary basin in the north, east-west banded, with two thickness centers, Aksu region in northwest and Manjiaer-Kuruketage region in northeast and maximum thickness about 2 500−3 500 m. There are two sedimentary basins in the south, north-east banded, with two thickness centers, Yecheng and Hetian with maximum thickness about 1 500−2 000 m. The evolution of the basin can be divided into two stages, rift in Nanhuan (Cryogenian) and depression in Sinian (Ediacaran), the latter stage deposits larger range but with thinner thickness of strata. Its main rock types contain volcanic rock, clastic rock, moraine rock and carbonate rock. The distribution of source rock during Early Cambrian period is mainly controlled by the development characteristics of the Neoproterozoic sedimentary basin." @default.
• W2566385010 created "2017-01-06" @default.
• W2566385010 creator A5004675038 @default.
• W2566385010 creator A5048768379 @default.
• W2566385010 creator A5061602320 @default.
• W2566385010 creator A5062010629 @default.
• W2566385010 creator A5064350288 @default.
• W2566385010 creator A5069714324 @default.
• W2566385010 creator A5069741382 @default.
• W2566385010 date "2016-12-01" @default.
• W2566385010 modified "2023-10-18" @default.
• W2566385010 title "The characteristics of Precambrian sedimentary basin and the distribution of deep source rock: A case study of Tarim Basin in Neoproterozoic and source rocks in Early Cambrian, Western China" @default.
• W2566385010 cites W1971151083 @default.
• W2566385010 cites W2000606365 @default.
• W2566385010 cites W2005148268 @default.
• W2566385010 cites W2047738234 @default.
• W2566385010 cites W2048240400 @default.
• W2566385010 cites W2050582708 @default.
• W2566385010 cites W2076965374 @default.
• W2566385010 cites W2085249346 @default.
• W2566385010 cites W2090528531 @default.
• W2566385010 cites W2126275389 @default.
• W2566385010 cites W2130049175 @default.
• W2566385010 cites W2139894373 @default.
• W2566385010 cites W2143385549 @default.
• W2566385010 doi "https://doi.org/10.1016/s1876-3804(16)30116-1" @default.
• W2566385010 hasPublicationYear "2016" @default.
• W2566385010 type Work @default.
• W2566385010 sameAs 2566385010 @default.
• W2566385010 citedByCount "44" @default.
• W2566385010 countsByYear W25663850102017 @default.
• W2566385010 countsByYear W25663850102018 @default.
• W2566385010 countsByYear W25663850102019 @default.
• W2566385010 countsByYear W25663850102020 @default.
• W2566385010 countsByYear W25663850102021 @default.
• W2566385010 countsByYear W25663850102022 @default.
• W2566385010 countsByYear W25663850102023 @default.
• W2566385010 crossrefType "journal-article" @default.
• W2566385010 hasAuthorship W2566385010A5004675038 @default.
• W2566385010 hasAuthorship W2566385010A5048768379 @default.
• W2566385010 hasAuthorship W2566385010A5061602320 @default.
• W2566385010 hasAuthorship W2566385010A5062010629 @default.
• W2566385010 hasAuthorship W2566385010A5064350288 @default.
• W2566385010 hasAuthorship W2566385010A5069714324 @default.
• W2566385010 hasAuthorship W2566385010A5069741382 @default.
• W2566385010 hasBestOaLocation W25663850101 @default.
• W2566385010 hasConcept C109007969 @default.
• W2566385010 hasConcept C114793014 @default.
• W2566385010 hasConcept C120806208 @default.
• W2566385010 hasConcept C126559015 @default.
• W2566385010 hasConcept C127313418 @default.
• W2566385010 hasConcept C138170599 @default.
• W2566385010 hasConcept C147717901 @default.
• W2566385010 hasConcept C151730666 @default.
• W2566385010 hasConcept C169212394 @default.
• W2566385010 hasConcept C173776410 @default.
• W2566385010 hasConcept C17409809 @default.
• W2566385010 hasConcept C192241223 @default.
• W2566385010 hasConcept C200646496 @default.
• W2566385010 hasConcept C2779241739 @default.
• W2566385010 hasConcept C2780049196 @default.
• W2566385010 hasConcept C2780321876 @default.
• W2566385010 hasConcept C50682988 @default.
• W2566385010 hasConcept C6494504 @default.
• W2566385010 hasConcept C77928131 @default.
• W2566385010 hasConceptScore W2566385010C109007969 @default.
• W2566385010 hasConceptScore W2566385010C114793014 @default.
• W2566385010 hasConceptScore W2566385010C120806208 @default.
• W2566385010 hasConceptScore W2566385010C126559015 @default.
• W2566385010 hasConceptScore W2566385010C127313418 @default.
• W2566385010 hasConceptScore W2566385010C138170599 @default.
• W2566385010 hasConceptScore W2566385010C147717901 @default.
• W2566385010 hasConceptScore W2566385010C151730666 @default.
• W2566385010 hasConceptScore W2566385010C169212394 @default.
• W2566385010 hasConceptScore W2566385010C173776410 @default.
• W2566385010 hasConceptScore W2566385010C17409809 @default.
• W2566385010 hasConceptScore W2566385010C192241223 @default.
• W2566385010 hasConceptScore W2566385010C200646496 @default.
• W2566385010 hasConceptScore W2566385010C2779241739 @default.
• W2566385010 hasConceptScore W2566385010C2780049196 @default.
• W2566385010 hasConceptScore W2566385010C2780321876 @default.
• W2566385010 hasConceptScore W2566385010C50682988 @default.
• W2566385010 hasConceptScore W2566385010C6494504 @default.
• W2566385010 hasConceptScore W2566385010C77928131 @default.
• W2566385010 hasIssue "6" @default.
• W2566385010 hasLocation W25663850101 @default.
• W2566385010 hasOpenAccess W2566385010 @default.
• W2566385010 hasPrimaryLocation W25663850101 @default.
• W2566385010 hasRelatedWork W1550844290 @default.
• W2566385010 hasRelatedWork W1970916739 @default.
• W2566385010 hasRelatedWork W2052478227 @default.
• W2566385010 hasRelatedWork W2366082373 @default.
• W2566385010 hasRelatedWork W2376319851 @default.
• W2566385010 hasRelatedWork W2574972105 @default.
• W2566385010 hasRelatedWork W2961064724 @default.
• W2566385010 hasRelatedWork W3139303661 @default.
• W2566385010 hasRelatedWork W3207513357 @default.
• W2566385010 hasRelatedWork W4200458400 @default.

• next