Tectonic evolution of the Qinling orogen, China: Review and synthesis

Dong, Yunpeng; Zhang, Guowei; Neubauer, Franz; Liu, Xiaoming; Genser, Johann; Hauzenberger, Christoph

doi:10.1016/j.jseaes.2011.03.002

Cited by 973 publications

(722 citation statements)

References 70 publications

(151 reference statements)

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“…The geomorphology and paleoecology of the QM were affected by various orogenic and climatic fluctuations (Zhou 2000;Dong et al 2011). During the late Miocene, the rapid uplift of the Tibetan Plateau has profoundly changed the geographical features of its adjacent regions, including the WQM (Zhang et al 2006), and driven the beginning of the Asia monsoons Molnar 2005).…”

Section: Prolonged Divergence and Multiple Glacial Refugiamentioning

confidence: 99%

“…Historically, drastic tectonic events, such as the significant uplifts of the Tibetan Plateau from the late Miocene, Kun-Huang diastrophisms, and Gonghe movements during the early Pleistocene, led to the development of the Mountains and valleys in the QM region Zhang et al 2006;Dong et al 2011). In addition, some high Mountains (e.g., Taibai mountain) greater than 3,000 m above sea level (a.s.l.)…”

Section: Introductionmentioning

confidence: 99%

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Phylogeographic Patterns of mtDNA Variation Revealed Multiple Glacial Refugia for the Frog Species Feirana taihangnica Endemic to the Qinling Mountains

et al. 2013

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Diversification patterns and demography of montane species are affected by Pleistocene climate fluctuations. Empirical cases from the Qinling Mountains (QM) region, which is a major biogeographic divider of East Asia, are few. We used DNA sequence data of the complete mitochondrial ND2 gene to detect effects of the Pleistocene glaciations on phylogeographic profiles of a frog species, Feirana taihangnica, which is endemic to the QM. Four distinct lineages consisting of seven sublineages were revealed. The strongest signal of biogeographical structure (F ct = 0.971, P \ 0.01) was found when populations were grouped according to these seven sublineages. One narrow secondary contact zone was detected in the middle QM between the lineage from middle QM and the lineage from eastern QM. Coalescent simulations indicated that this species colonized the QM region by a stepping-stone model. Divergences among lineages had likely been influenced by the uplift of the Tibetan Plateau during the late Miocene-tolate Pleistocene, as well as by the Pleistocene climatic cycles. Coalescent simulations also suggested that F. taihangnica populations have persisted through the Pleistocene glacial periods in multiple refugia across the QM region. Demographic analyses indicated that all lineages, except the lineage in the Funiu Mountains, have been experienced postglacial expansion of population size and distribution range. In conclusion, Pleistocene climate fluctuations and tectonic changes during the late Miocene-late Pleistocene have profoundly influenced the phylogeography and historical demography of F. taihangnica.

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Section: Prolonged Divergence and Multiple Glacial Refugiamentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Phylogeographic Patterns of mtDNA Variation Revealed Multiple Glacial Refugia for the Frog Species Feirana taihangnica Endemic to the Qinling Mountains

et al. 2013

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“…During the Mesozoic, the basin developed in an intracratonic setting (Liu et al, 2008). The late Triassic records the climax of the main orogenic episode in the evolution of the Qinling Mountains that bordered the southern margin of the Ordos Basin Li et al, 2007;Dong et al, 2011;Bao et al, 2014). Northward compression of the Qinling Orogen in the late Triassic is thought to have occurred as a series of pulses that drove cyclic subsidence of the southern part of the Ordos Basin and also delivered an abundant supply of clastic detritus to the subsiding basin as a response to each uplift episode (Liu, 1998(Liu, , 2000Yang, 2004;Li et al, 2007;Liu et al, 2008;Deng et al, 2013).…”

Section: Controls On Fluvio-lacustrine Delta Evolutionmentioning

confidence: 99%

Outcrop architecture of a fluvio-lacustrine succession: Upper Triassic Yanchang Formation, Ordos Basin, China

Zhao

Mountney

Liu

et al. 2015

Marine and Petroleum Geology

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Detailed analysis of the internal architectures of the delta-front bodies records the mechanism of growth of a large-scale, shallow-water delta succession. However, significant differences are identified in the development of this lacustrine delta compared to that of more commonly recognized marine shelf-edge delta systems.Lacustrine subaqueous distributary channels have 3 to 15 m-thick sandstone fills and 2 are more abundant and better developed than their marine counterparts: such channelized bodies are highly elongate and many can be traced several kilometres.Such bodies can be shown to be commonly associated with thin-bedded mouth-bar and subaqueous interdistributary-bay deposition. Overall, the Yanchang Formation is characterized by 4 major transgressive-regressive cycles, the development of which was controlled by a combination of changes in the rate of tectonic subsidence, the rate of sediment delivery from the basin margin hinterland and climate -factors that were themselves influenced by intracontinental growth of the neighbouring Qinling Orogen.

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“…그리고 그 이후 친링 충돌대에서 페름기말-트라이아 스기 대륙 충돌 이전에 고생대 중기의 대륙 충돌이 일어났음이 보고되었다 (Meng and Zhang, 2000;Dong et al, 2011;Shi et al, 2013). 아직 논란 중에 있기는 하나 고생대 중기의 대륙 충돌 작용은 남중국판과 북중국판 사이에 존재하였던 소대륙판인 북친링판(North Qinling block)과 남친링판(South Qinling block)이 북중국판과 충돌에 의해 발생된 것 으로 해석되고 있다 (Fig.…”

Section: 서 언unclassified

“…아직 논란 중에 있기는 하나 고생대 중기의 대륙 충돌 작용은 남중국판과 북중국판 사이에 존재하였던 소대륙판인 북친링판(North Qinling block)과 남친링판(South Qinling block)이 북중국판과 충돌에 의해 발생된 것 으로 해석되고 있다 (Fig. 1b;Meng and Zhang, 2000;Dong et al, 2011). 그리고 고생대 중기의 북 친링 소대륙판과 북중국판의 충돌대를 따라 충돌 후 화성암이 광역적으로 형성되었다( Fig.…”

Section: 서 언unclassified

Review on the Triassic Post-collisional Magmatism in the Qinling Collision Belt

Oh¹,

Lee²,

Yi³

et al. 2014

The Journal of the Petrological Society of Korea

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The Qinling-Dabie-Sulu-Hongseong-Odesan collision belt was formed by the collision between the North China and South China Cratons during late Permian to Triassic. During the collision, Triassic post-collision igneous rocks regionally intruded in the Qinling and the Hongseong-Odesan collision belts which represent the western and eastern ends of the collision belt, respectively. However, no and minor Triassic post-collision igneous activities occur in the Dabie and Sulu belts respectively. The peak metamorphic pressure conditions along the Qinling-Dabie-Sulu-Hongseong-Odesan belt indicate that the slab break-off occurred at the depth of ultra-high pressure (UHP) metamorphic condition in the Dabie and

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Tectonic evolution of the Qinling orogen, China: Review and synthesis

Cited by 973 publications

References 70 publications

Phylogeographic Patterns of mtDNA Variation Revealed Multiple Glacial Refugia for the Frog Species Feirana taihangnica Endemic to the Qinling Mountains

Phylogeographic Patterns of mtDNA Variation Revealed Multiple Glacial Refugia for the Frog Species Feirana taihangnica Endemic to the Qinling Mountains

Outcrop architecture of a fluvio-lacustrine succession: Upper Triassic Yanchang Formation, Ordos Basin, China

Review on the Triassic Post-collisional Magmatism in the Qinling Collision Belt

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