An Z S, Wu G X, Li J P, et al. 2015. Global monsoon dynamics and climate change. Annu Rev Earth Planet Sci, 43: 2.1–2.49
[3]
Molnar P. 1986b. The Structure of mountain ranges. Sci Am, 254: 70–79
[4]
Molnar P. 2004. Late Cenozoic increase in accumulation rates of terrestrial sediment: How might climate change have affected erosion rates? Annu Rev Earth Planet Sci, 32: 67–89
[5]
Molnar P. 2005. Mio-Pliocene growth of the Tibetan Plateau and evolution of east Asian climate. Palaeontol Electron, 8: 2A
[6]
Molnar P, England P. 1990. Late Cenozoic uplift of mountain ranges and global climatic change: Chicken or egg? Nature, 346: 29–34
[7]
Molnar P, Houseman G A. 2013. Rayleigh-Taylor instability, lithospheric dynamics, surface topography at convergent mountain belts, and gravity anomalies. J Geophys Res, 118: 2544–2557
[8]
Molnar P, Lyon-Caen H. 1989. Fault plane solutions of earthquakes and active tectonics of the Tibetan Plateau and its margins. Geophys J Int, 99: 123–153
[9]
Molnar P, Stock J M. 2009. Slowing of India''s convergence with Eurasia since 20 Ma and its implications for Tibetan mantle dynamics. Tectonics, 28: TC3001
[10]
Molnar P, Tapponnier P. 1975. Cenozoic tectonics of Asia: Effects of continental collision. Science, 189: 419–426
[11]
Molnar P, Tapponnier P. 1978. Active tectonics of Tibet. J Geophys Res, 83: 5361–5375
[12]
Molnar P, Boos W R, Battisti D S. 2010. Orographic controls on climate and paleoclimate of Asia: Thermal and mechanical roles for the Tibetan Plateau. Annu Rev Earth Planet Sci, 38: 77–102
[13]
Molnar P, Burchfiel B C, Zhao Z Y, et al. 1987. The geologic evolution of northern Tibet: Results from an expedition to Ulugh Muztagh. Science, 235: 299–304
[14]
Molnar P, England P, Martinod J. 1993. Mantle dynamics, the uplift of the Tibetan Plateau and the Indian monsoon. Rev Geophys, 31: 357–396
[15]
Molnar P, Houseman G A, England P C. 2006. Palaeo-altimetry of Tibet. Nature, 444: E4
[16]
Molnar P, Houseman G A, Conrad C P. 1998. Rayleigh-Taylor instability and convective thinning of mechanically thickened lithosphere: Effects of non-linear viscosity decreasing exponentially with depth and of horizontal shortening of the layer. Geophys J Int, 133: 568–584
[17]
Molnar P, Cane M A. 2007. Early pliocene (pre-Ice Age) El Nino-like global climate: Which El Nino? Geosphere, 3: 337–365
[18]
Ou J M, Du A M, Thebaulte E, et al. 2013. A high resolution lithospheric magnetic field model over China. Sci China Earth Sci, 56: 1759–1768
[19]
Philander S G, Fedorov A V. 2003. Role of tropics in changing the response to Milankovich forcing some three million years ago. Paleoceanography, 18: 1045
[20]
Raymo M E, Ruddiman W F. 1992. Tectonic forcing of late Cenozoic climate. Nature, 359: 117–122
[21]
Scharer U, Xu R H, Allegre C J. 1984. U-Pb geochronology of Gangdese (Transhimalaya) plutonism in the Lhasa-Xigaze region, Tibet. Earth Planet Sci Lett, 69: 311–320
Champagnac J D, Molnar P, Sue C, et al. 2012. Tectonics, climate, and mountain topography. J Geophys Res, 117: B02403
[42]
Chen J S, Huang B C, Sun L S. 2010. New constraints to the onset of the India-Asia collision: Paleomagnetic reconnaissance on the Linzizong Group in the Lhasa Block, China. Tectonophysics, 489: 189–209
[43]
Dayem K E, Molnar P, Battisti D S, et al. 2010. Lessons learned from oxygen isotopes in modern precipitation applied to interpretation of speleothem records of paleoclimate from eastern Asia. Earth Planet Sci Lett, 295: 219–230
[44]
Gan W J, Zhang P Z, Shen Z K, et al. 2007. Present-day crustal motion within the Tibetan Plateau inferred from GPS measurements. J Geophys Res, 112: B08416
[45]
Guo Z T, Ruddiman W F, Hao Q Z, et al. 2002. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature, 416: 159–163
[46]
Guo Z T, Sun B, Zhang Z S, et al. 2008. A major reorganization of Asian climate by the early Miocene. Clim Past, 4: 153–174
[47]
Laskar J, Robutel P, Joutel F, et al. 2004. A long-term numerical solution for the insolation quantities of the Earth. Astron Astrophys, 428: 261–285
[48]
Lu H Y, Wang X Y, Li L P. 2010. Aeolian sediment evidence that global cooling has driven late Cenozoic stepwise aridification in central Asia. In: Clift P D, Tada R, Zheng H, eds. Monsoon Evolution and Tectonics-Climate Linkage in Asia. Geol Soc London Spec Publ, 342: 29–44
[49]
Mao L G, Xiao A C, Wu L, et al. 2014. Cenozoic tectonic and sedimentary evolution of southern Qaidam Basin, NE Tibetan Plateau and its implication for the rejuvenation of Eastern Kunlun Mountains. Sci China Earth Sci, 57: 2726–2739
[50]
Molnar P. 1986a. The geologic history and structure of the Himalaya. Am Sci, 74: 144–154
[51]
Smith A G, Hurley A M, Briden J C. 1981. Phanerozoic Paleocontinential World Maps. Cambridge: Cambridge University Press
[52]
Sun J M, Xu Q H, Liu W M, et al. 2014. Palynological evidence for the latest Oligocene-early Miocene paleoelevation estimate in the Lunpola Basin, central Tibet. Paleogeogr Paleoclimatol Paleoecol, 399: 21–30
[53]
Tapponnier P, Molnar P. 1976. Slip-line field theory and large-scale continental tectonics. Nature, 264: 319–324
[54]
Tapponnier P, Xu Z Q, Roger F, et al. 2001. Oblique stepwise rise and growth of the Tibetan Plateau. Science, 294: 1671–1677
[55]
Tian J. 2013. Coherent variations of the obliquity components in global ice volume and ocean carbon reservoir over the past 5 Ma. Sci China Earth Sci, 56: 2160–2172
[56]
Wang C S, Zhao X X, Liu Z F, et al. 2008. Constraints on the early uplift history of the Tibetan Plateau. Proc Natl Acad Sci USA, 105: 4987–4992
[57]
Wang X F, Li R Y, Li X Z, et al. 2014. Variations in leaf characteristics of three species of angiosperms with changing of altitude in Qilian Mountains and their inland high-altitude pattern. Sci China Earth Sci, 57: 662–670
[58]
Wu G, Liu Y M, He B, et al. 2012. Thermal controls on the Asian Summer monsoon. Sci Rep, 2: 404
[59]
Xu Z Q, Wang Q, Arnaud P, et al. 2013. Orogen-parallel ductile extension and extrusion of the Greater Himalaya in the late Oligocene and Miocene. Tectonics, 32: 191–215
[60]
Yin A. 2006. Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation. Earth-Sci Rev, 76: 1–131
[61]
Zachos J C, Dickens G R, Zeebe R E. 2008. An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics. Nature, 451: 279–283
[62]
Zhang P Z. 2013. A review on active tectonics and deep crustal processes of the Western Sichuan region, eastern margin of the Tibetan Plateau. Tectonophysics, 584, 7–22
[63]
Zhang P Z, Molnar P, Downs W R. 2001. Increased sedimentation rates and grain sizes 2–4 Myr ago due to the influence of climate changes on erosion rates. Nature, 410: 891–897
[64]
Zhang P Z, Shen Z K, Burgman R, et al. 2004. Continuous deformation of the Tibetan Plateau constrained from Global Positioning measurements. Geology, 32: 809–812
[65]
Zhang Y G, Pagani M, Liu Z H. 2014. A 12-million-year temperature history of the tropical pacific ocean. Science, 344: 84–87
[66]
Zhao L, Zhao M, Lu G. 2014. Upper mantle seismic anisotropy beneath a convergent boundary: SKS waveform modeling in central Tibet. Sci China Earth Sci, 57: 759–776
