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• W2365401964 abstract "The ideas and concepts regarding to the analysis of syntectonic sedimentation are briefly introduced together with the investigation approaches and its potential implications to the research of regional tectonic deformation processes. It was studied that the tectonic deformations together with the conglomerate composition variation within the Late Jurassic Tuchengzi Formation in south of Lingyuan City, western Liaoning Province, the following conclusions are reached. (1) The syntectonic/synkinematic sedimentation in the research area was commenced after the volcanism of the Tiaojishan Formation. The provenance area was located to the west of the synkinematic sedimentary basin—Dengzhangzi Basin, instead of the east side of the basin. Dengzhangzi Basin was not a foredeep sedimentary basin of the westward thrusting as it was thought to be by previous investigators. Variations of the conglomerates within the Tuchengzi Formation indicate an erosion and unroofing sequence of the tilted normal sequence of the provenance strata. The erosion reached the upper part of the Wumishan Formation of the Mesoproterozoic Jixian Group. (2) The contacts between the relic slices of Mesoproterozoic Changcheng Group, lying between the Niuyingzi-Guojiadian Basin and the Dengzhangzi Bansin, and the Beipiao group to the east is a major east southeast-ward thrust fault. To the northwest side, however, the Tuchengzi Formation lies unconformably on top of the relics of Changcheng Group. In the area SE of Laohugou where the Changcheng Group disappeared, the Tuchengzi Formation lies directly on top of the Beipiao Formation. The relics of Changcheng Group between the two basins aforementioned is interpreted to be a klippe formed during an extensive east-south-east thrusting events of prior to the volcanic activity of Tiaojishan formation. (3) The thrusting deformation sequence in the south of Lingyuan City, western Liaoning Province, could be identified as follows: starting from a southward thrusting prior to the Early Jurassic Beipiao Formation (the Indosinian), then to the east-south-east ward thrusting before Tiaojishan Formation followed by a thrusting and associated folding with vergence to the southeast after Tiaojishan Formation, finally to the ending of contraction deformation with local thrusting deformation within the Early Cretaceous Jiufotang Formation. About 35% shortening within the covering sequence was achieved during the east-south-east thrusting and folding in the study area." @default.
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• W2365401964 date "2004-01-01" @default.
• W2365401964 modified "2023-09-25" @default.
• W2365401964 title "Syntectonic sedimentation analysis applied to the reconstructionof the thrusting deformation process: An example fromthe Mesozoic thrust tectonics in eastern Yanshan Orogenic Belt,south of Lingyuan City, western Liaoning Province" @default.
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