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| 1 | Magmatism during continental collision, subduction, exhumation and mountain collapse in collisional orogenic belts and continental net growth: A perspective显示文摘Continental orogens on Earth can be classified into accretionary orogen and collisional orogen.Magmatism in orogens occurs in every periods of an orogenic cycle,from oceanic subduction,continental collision to orogenic collapse.Continental collision requires the existence of prior oceanic subduction zone.It is generally assumed that the prerequisite of continental deep subduction is oceanic subduction and its drag force to the connecting passive-margin continental lithosphere during continental collision.Continental subduction and collision lead to the thickening and uplift of crust,but the formation time of the related magmatism in orogens depends on the heating mechanism of lithosphere.The accretionary orogens,on the other hand,have no strong continental collision,deep subduction,no large scale of crustal thrusting,thickening and uplift,and no UHP eclogite-facies metamorphic rocks related to continental deep subduction.Even though arc crust could be significantly thickened during oceanic subduction,it is still doubtful that syn-or post-collisional magmatism would be generated.In collisional orogens,due to continental deep subduction and significant crustal thickening,the UHP metamorphosed oceanic and continental crusts will experience decompression melting during exhumation,generating syn-collisional magmatism.During the orogen unrooting and collapse,post-collisional magmatism develops in response to lithosphere extension and upwelling of asthenospheric mantle,marking the end of an orogenic cycle.Therefore,magmatism in orogens can occur during the continental deep subduction,exhumation and uplift after detachment of subducted oceanic crust from continental crust,and extensional collapse.The time span from continental collision to collapse and erosion of orogens(the end of orogenic cycle)is 50–85 Myr.Collisional orogens are the key sites for understanding continental deep subduction,exhumation,uplift and orogenic collapse.Magmatism in collisional orogens plays important roles in continental reworking and net growth. | SONG ShuGuang WANG MengJue WANG Cao NIU YaoLing | 2015 | Science China Earth Sciences2015，58，8： | 39 |
| 2 | Qi-Qin Accretionary Belt in Central China Orogen: accretion by trench jam of oceanic plateau and formation of intra-oceanic arc in the Early Paleozoic Qin-Qi-Kun Ocean显示文摘Most orogenic belts have experienced a complex accretionary process with multiple episodes of sea?oor subduction and trench retreat.This accretionary process is important in continenta development and growth[1,2].Three giant orogens extend in China,e.g.,the Central Asian Orogen in the north,the Central China Orogen in the middle and the Himalayan Orogen in the southwest.They are keys for the formation of the Eurasian continent(Fig.1a).The Central China Orogen | Shuguang Song Liming Yang Yuqi Zhang Yaoling Niu Chao Wang Li Su Yanlin Gao | 2017 | Science Bulletin2017，62，15： | 28 |
| 3 | Tracing the 850-Ma continental flood basalts from a piece of subducted continental crust in the North Qaidam UHPM belt, NW China显示文摘 | Shuguang Song Li Su Xian-hua Li Guibing Zhang Yaoling Niu Lifei Zhang | 2010 | Precambrian Research2010，，4： | 2 |
| 4 | Geochronology of diamond-bearing zircons from garnet peridotite in the North Qaidam UHPM belt, Northern Tibetan Plateau: A record of complex histories from oceanic lithosphere subduction to continental collision显示文摘 | Shuguang Song Lifei Zhang Yaoling Niu Li Su Ping Jian Dunyi Liu | 2005 | Earth and Planetary Science Letters2005，，1： | 1 |
| 5 | Influence of ultrasonic vibration on mechanical properties and microstructure of 1Cr18Ni9Ti stainless steel显示文摘 | LIU Qingmei ZHANG Yong SONG Yaoling | 2006 | Materials & design2006，，： | 1 |
| 6 | Tectonic evolution of early Paleozoic HP metamorphic rocks in the North Qilian Mountains, NW China: New perspectives显示文摘 | Shuguang Song Yaoling Niu Lifei Zhang Chunjing Wei June G. Liou Li Su | 2008 | Journal of Asian Earth Sciences2008，，3： | 1 |
| 7 | Influence of ultrasonic vibration mechanical properties and microstructure of 1Cr18Ni9Ti stainless stell显示文摘 | Liu Qingmei Zhang Yong Song Yaoling | 2007 | Materials and Design2007，，28： | 1 |
| 8 | Metamorphism, anatexis, zircon ages and tectonic evolution of the Gongshan block inthe northern Indochina continent-An eastern extension of the Lhasa Block显示文摘 | Song Shuguang Niu Yaoling Wei Chunjing | 2010 | Lithos2010，120，34： | 1 |
| 9 | Tectonics of the North Qilian orogen, NW China显示文摘 | Shuguang Song Yaoling Niu Li Su Xiaohong Xia | 2012 | Gondwana Research2012，，： | 1 |
| 10 | The Origin, Evolution and Present State of Subcontinental Lithosphere——an IUGS-SECE conference显示文摘 | Yaoling Niu Shuguang Song Lifei Zhang | 2005 | Episodes2005，28，3： | 1 |
| 11 | Evolution from oceanic subduction to continental collision: a case study from the Northern Tibetan Plateau based on geochemical and geo- chronological data显示文摘 | Song Shuguang Zhang Lifei Niu Yaoling | 2006 | Journal of Petrology2006，47，3： | 1 |
| 12 | Tectonics of the North Qilian orogen, NW China 显示文摘 | Song Shuguang Niu Yaoling Su Li | 2013 | Gondwana Research2013，23，： | 1 |
| 13 | UHP metamorphic evolution of coesite-bearing eclogite from the Yuka terrane, North Qaidam UHPM belt, NW China显示文摘 | Zhang Guibin Ellis David J. Christy Andrew G. Zhang Lifei Niu Yaoling Song Shuguang | 2009 | European Journal of Mineralogy2009，，6： | 1 |
| 14 | Influence of ultrasonic vibration on mechanical properties and microstructure of 1CrlSNi9Ti stainless steel 显示文摘 | Liu Qingmei Zhang Yong Song Yaoling | 2007 | Materials and Design2007，28，6： | 1 |
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