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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Far East
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China
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Gansu China
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Hexi Corridor (1)
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Qilian Mountains (3)
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Qinling Mountains (1)
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Xizang China (2)
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Yunnan China (1)
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Tibetan Plateau (7)
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elements, isotopes
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carbon
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C-13/C-12 (1)
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isotope ratios (1)
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isotopes
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stable isotopes
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C-13/C-12 (1)
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O-18/O-16 (1)
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oxygen
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O-18/O-16 (1)
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geochronology methods
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(U-Th)/He (2)
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fission-track dating (2)
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thermochronology (2)
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geologic age
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Cenozoic
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Tertiary
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Neogene
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Miocene
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middle Miocene (6)
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upper Miocene (3)
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Pliocene
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lower Pliocene (1)
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Paleogene
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Eocene
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upper Eocene (1)
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Oligocene (1)
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igneous rocks
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igneous rocks
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plutonic rocks
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granites (1)
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metamorphic rocks
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metamorphic rocks (1)
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minerals
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phosphates
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apatite (4)
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silicates
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orthosilicates
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nesosilicates
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zircon group
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zircon (1)
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Primary terms
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absolute age (2)
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Asia
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Far East
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China
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Gansu China
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Hexi Corridor (1)
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Qilian Mountains (3)
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Qinling Mountains (1)
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Xizang China (2)
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Yunnan China (1)
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Tibetan Plateau (7)
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carbon
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C-13/C-12 (1)
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Cenozoic
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Tertiary
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Neogene
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Miocene
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middle Miocene (6)
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upper Miocene (3)
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Pliocene
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lower Pliocene (1)
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Paleogene
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Eocene
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upper Eocene (1)
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Oligocene (1)
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climate change (1)
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crust (1)
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deformation (4)
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faults (5)
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geochronology (2)
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igneous rocks
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plutonic rocks
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granites (1)
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isotopes
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stable isotopes
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C-13/C-12 (1)
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O-18/O-16 (1)
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metamorphic rocks (1)
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orogeny (3)
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oxygen
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O-18/O-16 (1)
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paleoclimatology (2)
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plate tectonics (1)
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sedimentary rocks
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clastic rocks
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sandstone (1)
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structural analysis (1)
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tectonics (6)
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sedimentary rocks
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sedimentary rocks
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clastic rocks
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sandstone (1)
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sedimentary structures
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channels (1)
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Cenozoic mountain building in eastern China and its correlation with reorganization of the Asian climate regime
Initial Cenozoic Exhumation of the Northern Chinese Tian Shan Deduced from Apatite (U-Th)/He Thermochronological Data
Channel Profile Response to Abrupt Increases in Mountain Uplift Rates: Implications for Late Miocene to Pliocene Acceleration of Intracontinental Extension in the Northern Qinling Range-Weihe Graben, Central China
Distinguishing tectonic versus climatic forcing on landscape evolution: An example from SE Tibetan Plateau
Multiproxy records in middle–late Miocene sediments from the Wushan Basin: Implications for climate change and tectonic deformation in the northeastern Tibetan Plateau
Mid-Miocene uplift of the northern Qilian Shan as a result of the northward growth of the northern Tibetan Plateau
Progressive northward growth of the northern Qilian Shan–Hexi Corridor (northeastern Tibet) during the Cenozoic
40 Ar/ 39 Ar Thermochronology on Central China Orogen: Cooling, uplift and implications for orogeny dynamics
Abstract 40 Ar/ 39 Ar geochronology was carried out on the non-deformed synorogenic granitoid plutons from the Qinling–Dabie Orogen. The new model cooling history (MCH) method is applied to K-feldspar to obtain information about its cooling history. MCH is a quicker and easier method of calculating cooling histories compared with the multi-domain diffusion (MDD) model. Cooling histories indicate that Qinling–Dabie suffered differential uplift and denudation processes since the collision in the Late Triassic. East Qinling uplifted and denuded rapidly from c. 181–187 to c. 150 Ma at a rate of c. 20 °C Ma −1 , three times as fast as west Qinling which was exhumed at a rate of c. 6.6 °C Ma −1 from c. 195–190 to c. 100 Ma. Although west and east Qinling started uplift and denudation at the same time, east Qinling reached the 150 °C geothermal line ( c. 7.5 km deep) at c. 150 Ma, earlier than west Qinling by c. 50 myr, suggesting that earliest collision and strongest compression occurred in east Qinling. Dabie is characterized with a polyphased process of uplift and denudation, implying that the subduction of south China block in this region was multi-staged. The emplacement of the granitoids and uplift pattern along Qinling–Dabie may be due to delamination of the root of the mountains or the slab break-off. Cooling histories suggest that more mass had been removed from the root of east Qinling than west Qinling and Dabie; the final delamination occurred in Dabie at c. 100 Ma but affected the whole Qinling–Dabie orogen.