Late Oligocene mountain building of the East Kunlun Shan in northeastern Tibet: Impact on the Cenozoic climate evolution in East Asia
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[1] D. Jiang,et al. Distinct effects of Tibetan Plateau growth and global cooling on the eastern and central Asian climates during the Cenozoic , 2022, Global and Planetary Change.
[2] Yibo Yang,et al. Reorganization of Asian climate in relation to Tibetan Plateau uplift , 2022, Nature Reviews Earth & Environment.
[3] C. Garzione,et al. Timing and mechanisms of Tibetan Plateau uplift , 2022, Nature Reviews Earth & Environment.
[4] P. Valdes,et al. The rise and demise of the Paleogene Central Tibetan Valley , 2022, Science advances.
[5] B. Windley,et al. Coupling between uplift of the Central Asian Orogenic Belt-NE Tibetan Plateau and accumulation of aeolian Red Clay in the inner Asia began at ~7 Ma , 2022, Earth-Science Reviews.
[6] Kexin Zhang,et al. Reconstruction of the latest Eocene-early Oligocene paleoenvironment in the Hoh Xil Basin (Central Tibet) based on palynological and ostracod records , 2021 .
[7] D. Zheng,et al. Topographic growth of the northeastern Tibetan Plateau during the middle‐late Miocene: Insights from integrated provenance analysis in the NE Qaidam Basin , 2021 .
[8] L. Ding,et al. Low-temperature thermochronology constraints on the evolution of the Eastern Kunlun Range, northern Tibetan Plateau , 2021, Geosphere.
[9] D. Jiang,et al. Effects of Tibetan Plateau Growth, Paratethys Sea Retreat and Global Cooling on the East Asian Climate by the Early Miocene , 2021, Geochemistry, Geophysics, Geosystems.
[10] D. Zheng,et al. Late Oligocene Tectonic Uplift of the East Kunlun Shan: Expansion of the Northeastern Tibetan Plateau , 2021, Geophysical Research Letters.
[11] E. al.,et al. Extreme Quaternary plate boundary exhumation and strike slip localized along the southern Fairweather fault, Alaska, USA , 2021, Geology.
[12] P. Valdes,et al. Orographic evolution of northern Tibet shaped vegetation and plant diversity in eastern Asia , 2021, Science Advances.
[13] Chengshan Wang,et al. Revised chronology of central Tibet uplift (Lunpola Basin) , 2020, Science Advances.
[14] Zhonghui Liu,et al. Cenozoic moisture fluctuations on the northeastern Tibetan Plateau and association with global climatic conditions , 2020 .
[15] Hong Chang,et al. The Cenozoic Evolution of Crustal Shortening and Left‐Lateral Shear in the Central East Kunlun Shan: Implications for the Uplift History of the Tibetan Plateau , 2020, Tectonics.
[16] Weibin Zhang,et al. Multiple Phases of Mountain Building on the Northern Tibetan Margin , 2020 .
[17] Chengshan Wang,et al. Late Eocene–Oligocene High Relief Paleotopography in the North Central Tibetan Plateau: Insights From Detrital Zircon U–Pb Geochronology and Leaf Wax Hydrogen Isotope Studies , 2020, Tectonics.
[18] C. Gautheron,et al. Innovations in (U–Th)/He, Fission Track, and Trapped Charge Thermochronometry with Applications to Earthquakes, Weathering, Surface‐Mantle Connections, and the Growth and Decay of Mountains , 2019, Tectonics.
[19] M. Fox,et al. Miocene Range Growth Along the Altyn Tagh Fault: Insights From Apatite Fission Track and (U‐Th)/He Thermochronometry in the Western Danghenan Shan, China , 2019, Journal of Geophysical Research: Solid Earth.
[20] L. Ding,et al. Mesozoic-Cenozoic evolution of the Eastern Kunlun Range, central Tibet, and implications for basin evolution during the Indo-Asian collision , 2019, Lithosphere.
[21] D. Stockli,et al. Tectonics of the Eastern Kunlun Range: Cenozoic Reactivation of a Paleozoic‐Early Mesozoic Orogen , 2019, Tectonics.
[22] Chong Xu,et al. Parallelism between the maximum exhumation belt and the Moho ramp along the eastern Tibetan Plateau margin: Coincidence or consequence? , 2019, Earth and Planetary Science Letters.
[23] G. Gehrels,et al. Cenozoic basin evolution of the central Tibetan plateau as constrained by U-Pb detrital zircon geochronology, sandstone petrology, and fission-track thermochronology , 2019, Tectonophysics.
[24] J. Saylor,et al. Magnetic polarity stratigraphy, provenance, and paleoclimate analysis of Cenozoic strata in the Qaidam Basin, NE Tibetan Plateau , 2019, GSA Bulletin.
[25] Majie Fan,et al. Carbonate stable and clumped isotopic evidence for late Eocene moderate to high elevation of the east-central Tibetan Plateau and its geodynamic implications , 2018, GSA Bulletin.
[26] H. Sinclair,et al. Spatial correlation bias in late-Cenozoic erosion histories derived from thermochronology , 2018, Nature.
[27] A. Yin,et al. Late Cenozoic magmatic inflation, crustal thickening, and >2 km of surface uplift in central Tibet , 2018 .
[28] E. Kirby,et al. Expansion of the Tibetan Plateau during the Neogene , 2017, Nature Communications.
[29] Junliang Ji,et al. High-resolution magnetostratigraphic study of the Paleogene-Neogene strata in the Northern Qaidam Basin: Implications for the growth of the Northeastern Tibetan Plateau , 2017 .
[30] R. Zhu,et al. Differential growth of the northern Tibetan margin: evidence for oblique stepwise rise of the Tibetan Plateau , 2017, Scientific Reports.
[31] B. He. Influences of elevated heating effect by the Himalaya on the changes in Asian summer monsoon , 2017, Theoretical and Applied Climatology.
[32] Peizhen Zhang,et al. Pulsed growth of the West Qinling at ~30 Ma in northeastern Tibet: Evidence from Lanzhou Basin magnetostratigraphy and provenance , 2016 .
[33] R. Zhu,et al. Relief history and denudation evolution of the northern Tibet margin: Constraints from 40Ar/39Ar and (U–Th)/He dating and implications for far-field effect of rising plateau , 2016 .
[34] X. Fang,et al. A Late-Eocene palynological record from the Hoh Xil Basin, northern Tibetan Plateau, and its implications for stratigraphic age, paleoclimate and paleoelevation , 2016 .
[35] Glendon S. Wu,et al. Cenozoic architecture and structural development of the eastern Qaidam basin , 2016 .
[36] Zhaojie Guo,et al. Source to sink relation between the Eastern Kunlun Range and the Qaidam Basin, northern Tibetan Plateau, during the Cenozoic , 2015 .
[37] R. Tada,et al. Late Oligocene–early Miocene birth of the Taklimakan Desert , 2015, Proceedings of the National Academy of Sciences.
[38] Fei Wang,et al. Cenozoic record of aeolian sediment accumulation and aridification from Lanzhou, China, driven by Tibetan Plateau uplift and global climate , 2014 .
[39] J. Spotila,et al. Insights from low‐temperature thermochronometry into transpressional deformation and crustal exhumation along the San Andreas fault in the western Transverse Ranges, California , 2013 .
[40] Marin K. Clark,et al. Low‐temperature thermochronometry along the Kunlun and Haiyuan Faults, NE Tibetan Plateau: Evidence for kinematic change during late‐stage orogenesis , 2013 .
[41] Chengshan Wang,et al. Multi-stage tectono-magmatic events of the Eastern Kunlun Range, northern Tibet: Insights from U-Pb geochronology and (U-Th)/He thermochronology , 2013 .
[42] L. Ding,et al. Paleogene high elevations in the Qiangtang Terrane, central Tibetan Plateau , 2013 .
[43] E. Kirby,et al. Two-phase growth of high topography in eastern Tibet during the Cenozoic , 2012 .
[44] Xiao-dong Liu,et al. Modeling the climate effects of different subregional uplifts within the Himalaya-Tibetan Plateau on Asian summer monsoon evolution , 2012 .
[45] Alan G. Jones,et al. Penetration of crustal melt beyond the Kunlun Fault into northern Tibet , 2012 .
[46] M. Clark. Continental collision slowing due to viscous mantle lithosphere rather than topography , 2012, Nature.
[47] Kerry Gallagher,et al. Transdimensional inverse thermal history modeling for quantitative thermochronology , 2012 .
[48] M. Brandon,et al. Topographic evolution of the Sierra Nevada measured directly by inversion of low-temperature thermochronology , 2012, American Journal of Science.
[49] R. Ketcham,et al. Accounting for long alpha-particle stopping distances in (U–Th–Sm)/He geochronology: Refinement of the baseline case , 2011 .
[50] Wenjin Zhao,et al. Injection of Tibetan crust beneath the south Qaidam Basin: Evidence from INDEPTH IV wide‐angle seismic data , 2011 .
[51] Chengshan Wang,et al. A mid-crustal strain-transfer model for continental deformation: A new perspective from high-resolution deep seismic-reflection profiling across NE Tibet , 2011 .
[52] Jie Chen,et al. Late Miocene-Pliocene deceleration of dextral slip between Pamir and Tarim: Implications for Pamir orogenesis , 2011 .
[53] Weijian Zhou,et al. New eolian red clay sequence on the western Chinese Loess Plateau linked to onset of Asian desertification about 25 Ma ago , 2011 .
[54] E. Kirby,et al. Millennial slip rates along the eastern Kunlun fault: Implications for the dynamics of intracontinental deformation in Asia , 2010 .
[55] K. Farley,et al. Early Cenozoic faulting of the northern Tibetan Plateau margin from apatite (U–Th)/He ages , 2010 .
[56] W. Boos,et al. Orographic controls on climate and paleoclimate of Asia: thermal and mechanical roles for the Tibetan Plateau. , 2010 .
[57] K. Farley,et al. Tectonic control on southern Sierra Nevada topography, California , 2009 .
[58] Brian S. Currie,et al. Paleoaltimetry of the Tibetan Plateau from D/H ratios of lipid biomarkers , 2009 .
[59] Wenjin Zhao,et al. Late Oligocene-Early Miocene thrusting in southern East Kunlun Mountains, northern Tibetan plateau , 2009 .
[60] S. Graham,et al. Stable isotopic constraints on the tectonic, topographic, and climatic evolution of the northern margin of the Tibetan Plateau , 2009 .
[61] K. Farley,et al. Apatite (U-Th)/He thermochronometry using a radiation damage accumulation and annealing model , 2009 .
[62] Q. Hao,et al. A major reorganization of Asian climate by the early Miocene , 2008 .
[63] A. Yin,et al. Cenozoic tectonic evolution of the Qaidam basin and its surrounding regions (Part 3): Structural geology, sedimentation, and regional tectonic reconstruction , 2008 .
[64] Chengshan Wang,et al. Constraints on the early uplift history of the Tibetan Plateau , 2008, Proceedings of the National Academy of Sciences.
[65] E. Kirby,et al. Slip rate gradients along the eastern Kunlun fault , 2007 .
[66] B. Fu,et al. Displacement and timing of left-lateral faulting in the Kunlun Fault Zone, northern Tibet, inferred from geologic and geomorphic features , 2007 .
[67] P. DeCelles,et al. High and dry in central Tibet during the Late Oligocene , 2007 .
[68] A. Yin,et al. Cenozoic tectonic evolution of Qaidam basin and its surrounding regions (part 2): Wedge tectonics in southern Qaidam basin and the Eastern Kunlun Range , 2007 .
[69] Wang Shicheng,et al. Apatite fission track evidence for Neogene uplift in the eastern Kunlun Mountains, northern Qinghai-Tibet Plateau, China , 2006 .
[70] A. Basu,et al. Source of Oligocene to Pliocene sedimentary rocks in the Linxia basin in northeastern Tibet from Nd isotopes: Implications for tectonic forcing of climate , 2005 .
[71] Pinxian Wang,et al. How old is the Asian monsoon system?—Palaeobotanical records from China , 2005 .
[72] K. Farley,et al. A precise 40Ar–39Ar reference age for the Durango apatite (U–Th)/He and fission-track dating standard , 2005 .
[73] Peizhen Zhang,et al. Continuous deformation of the Tibetan Plateau from global positioning system data , 2004 .
[74] Qiu Nansheng,et al. Geothermal regime in the Qaidam basin, northeast Qinghai–Tibet Plateau , 2003, Geological Magazine.
[75] J. Malavieille,et al. Neogene extension and volcanism in the Kunlun Fault Zone, northern Tibet: New constraints on the age of the Kunlun Fault , 2003 .
[76] X. Fang,et al. Flexural subsidence by 29 Ma on the NE edge of Tibet from the magnetostratigraphy of Linxia Basin, China , 2003 .
[77] P. Tapponnier,et al. Seismic evidence for stepwise thickening of the crust across the NE Tibetan plateau , 2002 .
[78] Shuzhen Peng,et al. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China , 2002, Nature.
[79] M. Caffee,et al. Uniform postglacial slip-rate along the central 600 km of the Kunlun Fault (Tibet), from 26Al, 10Be, and 14C dating of riser offsets, and climatic origin of the regional morphology , 2002 .
[80] Chengshan Wang,et al. Tertiary crustal shortening and peneplanation in the Hoh Xil region: implications for the tectonic history of the northern Tibetan Plateau , 2002 .
[81] K. Farley,et al. (U-Th)/He Dating of Phosphates: Apatite, Monazite, and Xenotime , 2002 .
[82] Bertrand Meyer,et al. Oblique Stepwise Rise and Growth of the Tibet Plateau , 2001, Science.
[83] J. Kutzbach,et al. Evolution of Asian monsoons and phased uplift of the Himalaya–Tibetan plateau since Late Miocene times , 2001, Nature.
[84] An Yin,et al. Geologic Evolution of the Himalayan-Tibetan Orogen , 2000 .
[85] N. Arnaud,et al. An early unroofing in northeastern Tibet? Constraints from 40Ar/39Ar thermochronology on granitoids from the eastern Kunlun range (Qianghai, NW China) , 1999 .
[86] Bertrand Meyer,et al. Crustal thickening in Gansu‐Qinghai, lithospheric mantle subduction, and oblique, strike‐slip controlled growth of the Tibet plateau , 1998 .
[87] Peter Molnar,et al. Mantle dynamics, uplift of the Tibetan Plateau, and the Indian Monsoon , 1993 .