FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2956308004> ?p ?o ?g. }

• W2956308004 endingPage "71" @default.
• W2956308004 startingPage "57" @default.
• W2956308004 abstract "In order to unravel the Mesozoic sedimentation in response to multistage deformation of the western Ordos fold-thrust belt, combined zircon U-Pb and fission track analyses of single zircon grain are conducted for seven sandstone samples in the Helanshan area. Zircon FT ages are calculated using absolute uranium concentration determined by LA-ICP-MS during the procedure of zircon U-Pb dating. The newly-obtained zircon FT data show age features that are comparable with the previous zircon FT ages obtained by conventional FT methods (by which uranium contents are determined through an external detector to map induced fission tracks). The newly-obtained zircon FT ages have four subordinate FT age peaks (i.e., 225 Ma, 165 Ma, 125 Ma and 80 Ma) which are well matched with the regional geodynamic events occurred in the Late Triassic, Late Jurassic, Late Cretaceous and Early Cenozoic, respectively; and the zircon U-Pb ages have two main peaks at the Paleoproterozoic and the Late Paleozoic. The zircon U-Pb ages, integrating with the FT ages and available paleocurrents, suggest that the Paleoproterozoic basement rocks and Late Paleozoic plutonic rocks of the Alxa Block are the source rocks for the Triassic sandstones, and the Jurassic sandstones are associated with a multi-cycling sedimentation. The Jurassic sandstones contain recycled zircons that firstly deposited in the Triassic strata and subsequently exhumed during the Late Triassic-Early Jurassic." @default.
• W2956308004 created "2019-07-23" @default.
• W2956308004 creator A5006419646 @default.
• W2956308004 creator A5022178399 @default.
• W2956308004 creator A5027938145 @default.
• W2956308004 creator A5053772918 @default.
• W2956308004 creator A5071466437 @default.
• W2956308004 creator A5071679178 @default.
• W2956308004 creator A5075723798 @default.
• W2956308004 date "2019-10-01" @default.
• W2956308004 modified "2023-10-15" @default.
• W2956308004 title "Combined detrital zircon fission track and U-Pb dating of the Late Paleozoic to Early Mesozoic sandstones in the Helanshan, western Ordos fold-thrust belt: Constraints for provenance and exhumation history" @default.
• W2956308004 cites W1562583789 @default.
• W2956308004 cites W1596443511 @default.
• W2956308004 cites W1809106123 @default.
• W2956308004 cites W1973926757 @default.
• W2956308004 cites W1974688443 @default.
• W2956308004 cites W1982643048 @default.
• W2956308004 cites W1984617079 @default.
• W2956308004 cites W1985274828 @default.
• W2956308004 cites W1985699465 @default.
• W2956308004 cites W1986886630 @default.
• W2956308004 cites W1987496641 @default.
• W2956308004 cites W1990263716 @default.
• W2956308004 cites W2000602051 @default.
• W2956308004 cites W2017370529 @default.
• W2956308004 cites W2023965697 @default.
• W2956308004 cites W2024202801 @default.
• W2956308004 cites W2028042452 @default.
• W2956308004 cites W2029464449 @default.
• W2956308004 cites W2033515082 @default.
• W2956308004 cites W2040380547 @default.
• W2956308004 cites W2043592691 @default.
• W2956308004 cites W2044938074 @default.
• W2956308004 cites W2047155676 @default.
• W2956308004 cites W2048230691 @default.
• W2956308004 cites W2049355918 @default.
• W2956308004 cites W2060866316 @default.
• W2956308004 cites W2065352141 @default.
• W2956308004 cites W2066222850 @default.
• W2956308004 cites W2068892745 @default.
• W2956308004 cites W2070836124 @default.
• W2956308004 cites W2074493558 @default.
• W2956308004 cites W2074761424 @default.
• W2956308004 cites W2079604593 @default.
• W2956308004 cites W2085401740 @default.
• W2956308004 cites W2088558398 @default.
• W2956308004 cites W2091435387 @default.
• W2956308004 cites W2105119747 @default.
• W2956308004 cites W2106814179 @default.
• W2956308004 cites W2115505983 @default.
• W2956308004 cites W2116351028 @default.
• W2956308004 cites W2127755626 @default.
• W2956308004 cites W2133500098 @default.
• W2956308004 cites W2133656929 @default.
• W2956308004 cites W2136949069 @default.
• W2956308004 cites W2139096563 @default.
• W2956308004 cites W2142747196 @default.
• W2956308004 cites W2171086159 @default.
• W2956308004 cites W2233605606 @default.
• W2956308004 cites W2263311395 @default.
• W2956308004 cites W2306408647 @default.
• W2956308004 cites W2325963710 @default.
• W2956308004 cites W2567790362 @default.
• W2956308004 cites W2611632140 @default.
• W2956308004 cites W2735817365 @default.
• W2956308004 cites W2743280741 @default.
• W2956308004 cites W2751277630 @default.
• W2956308004 cites W2770302581 @default.
• W2956308004 cites W2777940559 @default.
• W2956308004 cites W2788851455 @default.
• W2956308004 cites W2797281763 @default.
• W2956308004 cites W2800186782 @default.
• W2956308004 cites W2803674437 @default.
• W2956308004 cites W2887636044 @default.
• W2956308004 cites W2915121365 @default.
• W2956308004 doi "https://doi.org/10.1016/j.jog.2019.07.001" @default.
• W2956308004 hasPublicationYear "2019" @default.
• W2956308004 type Work @default.
• W2956308004 sameAs 2956308004 @default.
• W2956308004 citedByCount "7" @default.
• W2956308004 countsByYear W29563080042021 @default.
• W2956308004 countsByYear W29563080042022 @default.
• W2956308004 countsByYear W29563080042023 @default.
• W2956308004 crossrefType "journal-article" @default.
• W2956308004 hasAuthorship W2956308004A5006419646 @default.
• W2956308004 hasAuthorship W2956308004A5022178399 @default.
• W2956308004 hasAuthorship W2956308004A5027938145 @default.
• W2956308004 hasAuthorship W2956308004A5053772918 @default.
• W2956308004 hasAuthorship W2956308004A5071466437 @default.
• W2956308004 hasAuthorship W2956308004A5071679178 @default.
• W2956308004 hasAuthorship W2956308004A5075723798 @default.
• W2956308004 hasConcept C109007969 @default.
• W2956308004 hasConcept C12294951 @default.
• W2956308004 hasConcept C127313418 @default.
• W2956308004 hasConcept C13106087 @default.
• W2956308004 hasConcept C151730666 @default.
• W2956308004 hasConcept C166957645 @default.

• next