FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2367191439> ?p ?o ?g. }

• W2367191439 abstract "The corresponding construction and transformation features remain in the shallow crust deposition and tectonic deformation during the destruction progress of North China Craton (NCC). On the basis of previous researches and the features of stratigraphic distribution, sedimentary and tectonic deformation, which are revealed by well drill, seismic profile and outcrop data. This paper discusses the response relationship between sedimentary basin prototype of the NCC and the early tectonic deformation of Craton destruction. During Late Triassic, the residual formation was in the characteristic of banded distribution: (1) the Upper Triassic Yanchang Formation develops well in the Ordos basin, the center of the NCC, and it extended eastward to central Shanxi and western Henan area; (2) the Upper Triassic Xingshikou Formation (and the contemporaneous Laohugou Formation and Heishanyao Formations) on the northern margin of the craton distributed sporadically along the line of western Liaoning—western Beijing—northern Hebei; (3) on southern margin of the craton, the Upper Triassic developed in the northern Qinling area, along the line of southern Henan—Southern Shaanxi. Both the Upper Triassic in the northern and southern margins of the craton had been involved into contemporaneous and deuteric tectonic deformation, most of the formations had been clamped by thrust faults and produced in the shape of fragment. From the perspective of tectonic deformation, Late Triassic large-scale S—N trending compressional structures had been discovered on both margins of the NCC, and they had formed Hedge patterns, which was in consistent with the existed E—W structure lines in intracraton. Syngenetic deposition recorded the process of regional tectonic deformation and/or the information of uplift and denudation controlled by deformation or other causes. In the intracraton, the western Ordos area was stable in tectonics, had weak deformation, and more complete residual strata; the eastern area uplifted intensely, most of the Upper Triassic strata is absent; and the central part, between eastern and western area, is a sedimentary—tectonic buffering transition region. From the perspective of prototype basin reconstruction, the NCC in Late Triassic is an intracontinental basin with foreland basins on both northern and southern margins. The prototype of the central NCC is an inheritance intracraton basin which overlays on the Lower—Middle Triassic basin. The intracontinental foreland system on the northern margin of the NCC consists of the Yinshan—Yanshan wedge-top belt, Zhangjiakou—Chengde foredeep, Qingshuihe—Shanhaiguan fore-bulge and western Beijing—Liujiang back-bulge depozones; and the intracontinental foreland system on the southern margin consists of the northern Qinling wedge-top belt, Pingliang—Nanzhao foredeep, Huanxian—Huoqiu fore-bulge and Tongchuan—Jiyuan back-bulge depozones. Of them, the Tongchuan—Jiyuan and western Beijing—Liujiang back-bulge depozones can also be allocated into the intracraton basins." @default.
• W2367191439 created "2016-06-24" @default.
• W2367191439 creator A5074642572 @default.
• W2367191439 date "2012-01-01" @default.
• W2367191439 modified "2023-09-23" @default.
• W2367191439 title "Prototypes of Late Triassic Sedimentary Basins of North China Craton (NCC) and Deformation Pattern of Its Early Destruction" @default.
• W2367191439 hasPublicationYear "2012" @default.
• W2367191439 type Work @default.
• W2367191439 sameAs 2367191439 @default.
• W2367191439 citedByCount "1" @default.
• W2367191439 countsByYear W23671914392020 @default.
• W2367191439 crossrefType "journal-article" @default.
• W2367191439 hasAuthorship W2367191439A5074642572 @default.
• W2367191439 hasConcept C105492442 @default.
• W2367191439 hasConcept C109007969 @default.
• W2367191439 hasConcept C127313418 @default.
• W2367191439 hasConcept C147717901 @default.
• W2367191439 hasConcept C151730666 @default.
• W2367191439 hasConcept C169212394 @default.
• W2367191439 hasConcept C17409809 @default.
• W2367191439 hasConcept C2776698055 @default.
• W2367191439 hasConcept C2781229967 @default.
• W2367191439 hasConcept C6494504 @default.
• W2367191439 hasConcept C77928131 @default.
• W2367191439 hasConcept C83365034 @default.
• W2367191439 hasConceptScore W2367191439C105492442 @default.
• W2367191439 hasConceptScore W2367191439C109007969 @default.
• W2367191439 hasConceptScore W2367191439C127313418 @default.
• W2367191439 hasConceptScore W2367191439C147717901 @default.
• W2367191439 hasConceptScore W2367191439C151730666 @default.
• W2367191439 hasConceptScore W2367191439C169212394 @default.
• W2367191439 hasConceptScore W2367191439C17409809 @default.
• W2367191439 hasConceptScore W2367191439C2776698055 @default.
• W2367191439 hasConceptScore W2367191439C2781229967 @default.
• W2367191439 hasConceptScore W2367191439C6494504 @default.
• W2367191439 hasConceptScore W2367191439C77928131 @default.
• W2367191439 hasConceptScore W2367191439C83365034 @default.
• W2367191439 hasOpenAccess W2367191439 @default.
• W2367191439 hasRelatedWork W1973635153 @default.
• W2367191439 hasRelatedWork W1985945219 @default.
• W2367191439 hasRelatedWork W2002955926 @default.
• W2367191439 hasRelatedWork W2032860696 @default.
• W2367191439 hasRelatedWork W2037741674 @default.
• W2367191439 hasRelatedWork W2078436811 @default.
• W2367191439 hasRelatedWork W2106814179 @default.
• W2367191439 hasRelatedWork W2352826317 @default.
• W2367191439 hasRelatedWork W2353421141 @default.
• W2367191439 hasRelatedWork W2369998719 @default.
• W2367191439 hasRelatedWork W2370901210 @default.
• W2367191439 hasRelatedWork W2384504272 @default.
• W2367191439 hasRelatedWork W2385943509 @default.
• W2367191439 hasRelatedWork W2386095142 @default.
• W2367191439 hasRelatedWork W2753208042 @default.
• W2367191439 hasRelatedWork W2965718954 @default.
• W2367191439 hasRelatedWork W3008512174 @default.
• W2367191439 hasRelatedWork W3187080989 @default.
• W2367191439 hasRelatedWork W3197828585 @default.
• W2367191439 hasRelatedWork W751748142 @default.
• W2367191439 isParatext "false" @default.
• W2367191439 isRetracted "false" @default.
• W2367191439 magId "2367191439" @default.
• W2367191439 workType "article" @default.