地球科学与工程学院-尊龙凯时网址

从事岩石大地构造学研究，重点研究青藏高原和造山带，包括蛇绿岩，高压超高压变质岩石，火山岩，基性超基性岩及有关矿产，如铬铁矿等。

2021-2024 蛇绿岩型铬铁矿的形成过程和深部地质作用 国家自然科学基金专项重点项目

2018-2022 大洋地幔橄榄岩-铬铁矿中的金刚石和深地幔再循环的全球蛇绿岩记录 国际(地区)合作与交流项目

 2017  古巴蛇绿岩地幔岩和铬铁矿中的金刚石和深地幔物质再循环记录 应急管理项目

2016-2018 西藏雅江与班怒成矿带铬铁矿综合调查 地质调查项目

 2016  全球不同构造背景蛇绿岩地幔橄榄岩和铬铁矿中金刚石等超高压矿物的成因探讨 应急管理项目

2015-2019 金刚石与地幔物质循环  igcp-649项目(unesco-usgs资助)

2015-2017 青藏高原铬铁矿资源潜力综合评价和泽当岩体调查 地质矿产调查评价专项

2014-2016 青藏高原/古新特提斯洋盆的构造演化和铬铁矿成矿作用 地质调查项目

2011-2013 雅鲁藏布江蛇绿岩和铬铁矿的地质背景和成因 地质调查项目

2011-2013 青藏高原拉萨地体松多高压—超高压变质带及印支造山作用 地质调查项目

2010-2013 蛇绿岩地幔岩和铬铁矿中的异常矿物和深部地质作用 国家自然科学基金委员会重点项目

2009-2010 青藏高原南部特提斯缝合带的形成与演化 地质调查项目

2008-2012 大陆科学钻探选址与科学钻探实验项目 行业专项项目

2007-2010 中国巨型中央造山带的复合造山运动学 地质调查项目

2006-2008 青藏高原南部地幔岩和铬铁矿成因 地质调查项目

2006-2008 蛇绿岩铬铁矿中超高压地幔矿物群和地幔动研究 国际合作基金

杨经绥, 连东洋, 吴魏伟等. 2022, 蛇绿岩中铬铁矿研究的问题与思考. 地质学报. 96(5): 1608-1634.

rui, h.c., yang, j.s., zheng, j. p. et al. 2022, early cretaceous subduction initiation of the proto-caribbean plate: geochronological and geochemical evidence from gabbros of the moa-baracoa ophiolitic massif, eastern cuba. lithos. 418-419.

rui, h.c., yang, j.s., llanes-castro, a.i. et al. 2022. ti-poor high-al chromitites of the moa-baracoa ophiolitic massif (eastern cuba) formed in a nascent forearc mantle. ore geology reviews. 144, 104847.

yang, j.s., wu, w. w., lian, d. y. et al. 2021. peridotites, chromitites and diamonds in ophiolites. nature reviews earth & environment. 2(3): 198-212.

feng, g.y., yang, j.s., niu, x.l. et al 2021. formation processes and tectonic implications of mantle peridotites of the yushigou ophiolite in the north qilian orogenic belt, nw china. lithos. 100-401, 106430.

rui, h. c., yang, j.s., llanes-castro, a. i. et al. 2021. highly refractory harzburgites from the moa-baracoa ophiolitic massif, eastern cuba: insights into forearc mantle melt-rock interactions. lithos. 404–405, 106427.

杨经绥. 2020. 大洋地幔橄榄岩-铬铁矿中的金刚石和深地幔再循环. 地质力学学报. 26(5): 731-741.

xiong, f. h., yang, j.s., schertl, h. p. et al. 2020. multistage origin of dunite in the purang ophiolite, southern tibet, documented by composition, exsolution and li isotope characteristics of constituent minerals. european journal of mineralogy. 32(1): 187-207.

lian, d.y., yang, j.s.,, dilek, y. et al. 2020. precambrian zircons in chromitites of the cretaceous aladag ophiolite (turkey) indicate deep crustal recycling in oceanic mantle. precambrian research. 350.

yang, j.s., lian, d.y, robinson, p. t. et al. 2019. comment on “a shallow origin for diamonds in ophiolitic chromitites”. geology. 47(8), e475-e475.

xiong, f.h., meng, y.k., yang, j.s. et al. 2019. geochronology and petrogenesis of the mafic dykes from the purang ophiolite: implications for evolution of the western yarlung-tsangpo suture zone, southwestern tibet. geoscience frontiers, 11(1): 277-292.

wu, w.w., yang, j.s., wirth, r. et al. 2019. carbon and nitrogen isotopes and mineral inclusions in diamonds from chromitites of the mirdita ophiolite (albania) demonstrate recycling of oceanic crust into the mantle, american mineralogist. 2019, 104: 485-500.

wu, w.w, yang, j.s.,, dilek, y. et al. 2018. multiple episodes of melting, depletion, and enrichment of the tethyan mantle: petrogenesis of the peridotites and chromitites in the jurassic skenderbeu massif, mirdita ophiolite, albania. lithosphere. 10(1), 54-78.

lian, d.y., yang, j.s., wiedenbeck, m. et al. 2018. carbon and nitrogen isotope, and mineral inclusion studies on the diamonds from the pozanti-karsanti chromitite, turkey. contributions to mineralogy and petrology. 173(9):1-18.

lian, d.y., yang, j.s., dilek, y. et al. 2017. deep mantle origin and ultra-reducing conditions in podiform chromitite: diamond, moissanite, and other unusual minerals in podiform chromitites from the pozanti-karsanti ophiolite, southern turkey. american mineralogist. 102(5), 1101-1113.

zhang, r.y., yang, j.s., ernst, w.g. et al. 2016. discovery of in situ super-reducing, ultrahigh-pressure phases in the luobusa ophiolitic chromitites, tibet: new insights into the deep upper mantle and mantle transition zone. american mineralogist. 101(5-6): 1285-1294.

yang, j.s., robinson, p.t., delik, y. 2015. diamond-bearing ophiolites and their geological occurrence. episodes. 38(4), 344-364.

yang, j.s., meng, f.c., xu, x.z. et al. 2015. diamonds, native elements and metal alloys from chromitites of the ray-iz ophiolite of the polar urals. gondwana research. 27(2), 459-485.

yang, j.s., robinson, p. t., dilek, y. 2014. diamonds in ophiolites. elements. 10(2), 127-130.

杨经绥, 徐向珍, 白文吉等. 2014. 蛇绿岩型金刚石的特征. 岩石学报. 30(8), 2113-2124.

许志琴, 杨经绥, 李文昌等, 2013. 青藏高原中的古特提斯体制与增生造山作用. 岩石学报. 29(6), 1847-1860.

杨经绥, 许志琴, 段向东等. 2012. 缅甸密支那地区发现侏罗纪的ssz型蛇绿岩. 岩石学报. 28(6): 1710-1730.

许志琴, 杨经绥, 李化启等. 2012. 中国大陆印支碰撞造山系及其造山机制. 岩石学报. 28(6): 1697-1709.

许志琴, 杨经绥, 李文昌等. 2012. 青藏高原南部与东南部重要成矿带的大地构造定格与找矿前景. 地质学报. 86(12): 1857-1868.

xu, x.z., yang, j.s., ba, d.z. et al. 2011.petrogenesis of the kangjinla peridotite in the luobusa ophiolite, southern tibet. journal of asia earth sciences. 42 (4), 553-568.

yang, j.s., li, t.f., chen, s.z. et al. 2009. genesis of garnet peridotites in the sulu uhp belt: examples from the ccsd-mh, pp1 and pp3 drillholes. tectonophysics. 475, 369-382

yang, j.s., xu, z.q., li, z.l. et al. 2009. discovery of an eclogite belt in the lhasa block, tibet: a new border for paleo-tethys? journal of asian earth sciences. 34, 76-89.

wu, c.l., yang, j.s., robinson, p.t. et al. 2009. geochemistry, age and tectonic significance of granitic rocks in north altun, northwest china. lithos. 113( 3-4): 423-436.

yang, j.s., dobrzhinetskaya, l., bai, w.j. et al. 2007. diamond- and coesite- bearing chromitites from the luobusa ophiolite, tibet. geology. 35(10), 875-878.

yang, j.s., zhang, r.y. , li, t.f. et al. 2007. petrogenesis of the garnet peridotite and garnet-free peridotite of the zhimafang ultramafic body in the sulu ultrahigh-pressure metamorphic belt, eastern china. journal of metamorphic geology. 25, 187-206.

li, z.l., yang, j.s., xu, z.q. et al. 2007. geochemistry, sm-nd and rb-sr isotopic compositions of eclogite in the lasha terrane, tibet, and their geological significance. geochimica et cosmochimica acta. 71(15): a577-a577.

yang, j.s., wu, c.l., zhang, j.x. et al. 2006. protolith of eclogites in the north qaidam and altun uhp terrane, nw china: earlier oceanic crust? journal of asian earth sciences. 28, 185-204.

xu, z.q., yang, j.s., wu, c.l. et al. 2006. timing and mechanism of formation and exhumation of the northern qaidam ultrahigh-pressure metamorphic belt. journal of asian earth sciences. 28, 160-173.

杨经绥, 李海兵. 2006. 走滑断裂对超高压变质岩石拆返的贡献及青藏高原北部白垩纪隆升之新思考. 地学前缘.13(4), 80-90

yang, j.s., liu, f.l., wu, c.l. et al. 2005. two ultrahigh-pressure metamorphic events recognized in the central orogenic belt of china: evidence from the u-pb dating of coesite-bearing zircons. international geology review. 47, 327-343

zhang, r.y., yang, j.s., wooden, j.l. et al. 2005. u-pb shrimp geochronology of zircon in garnet peridotite from the sulu uhp terrane, china: implications for mantle metasomatism and subduction-zone uhp metamorphism. earth and planetary science letters. 237, 729-743.

杨经绥, 史仁灯, 吴才来等. 2004. 柴达木盆地北缘新元古代蛇绿岩的厘定-罗迪尼亚大陆裂解的证据？地质通报. 23(9), 892-898.

史仁灯, 杨经绥, 吴才来等. 2004. 柴达木北缘超高压变质带中的岛弧火山岩. 地质通报.  78(1), 52-64.

史仁灯, 杨经绥，吴才来等.北祁连玉石沟蛇绿岩形成于晚震旦世的shrimp年龄证据. 地质通报.  78(5), 649-657.

吴才来, 杨经绥, 杨宏仪等. 2004. 北祁连东部两类i型花岗岩定年及其地质意义. 岩石学报. 20(3), 425-432.

yang, j.s., wooden, j.l., wu, c.l. et al. 2003. shrimp u-pb dating of coesite-bearing zircon from the ultrahigh-pressure metamorphic rocks, sulu terrane, east china. journal of metamorphic geology. 21, 551-560.

yang, j.s., xu, z.q., larissa, f. et al.2003. discovery of metamorphic diamonds in central china: an indication of a>4000-km-long zone of deep subduction resulting from multiple continental collisions. terra nova. 15, 370-379.

song, s.g., yang, j.s., liou, j.g. et al. 2003. petrology, eochemistry and isotopic ages of eclogites from the dulan uhpm terrane, the north qaidam, nw china. lithos. 70, 195-211.

song, s.g., yang, j.s., xu, z.q. et al. 2003. metamorphic evolution of the coesite-bearing ultrahigh-pressure terrane in the north qaidam, northern tibet, nw china. journal of metamorphic geology. 21, 631-644.

杨经绥, 刘福来, 吴才来等. 2003. 中央碰撞造山带中两期超高压变质作用: 来自含柯石英锆石的定年证据. 地质学报. 77(4), 463-477

杨经绥, 张建新, 孟繁聪等. 2003. 中国西部柴北缘—阿尔金的超高压变质榴辉及其原岩性质探讨. 地学前缘.10(3), 291-314

史仁灯, 杨经绥, 吴才来等. 2003. 柴北缘早古生代岛弧火山岩中埃达克质英安岩的发现及其地质意义. 岩石矿物学杂志. 22(3), 229-236

yang, j.s., xu, z.q., zhan, j.x. et al. 2002. early palaeozoic north qaidam uhp metamorphic belt on the north-eastern tibetan plateau and a paired subduction model. terra nova. 14(5), 397-404

杨经绥, 许志琴, 吴才来等. 2002. 含柯石英锆石的shrimp u-pb 定年: 胶东印支期超高压变质作用的证据.地质学报. 76(3), 354-372

张建新, 杨经绥, 许志琴等. 2002. 中国西北柴北缘两种不同类型榴辉岩. 地质学报. 76(3), 431

宋述光, 杨经绥. 2001. 柴达木盆地北缘都兰地区榴辉岩中透长石石英包裹体: 超高压变质作用的证据.地质学报. 75(2),180-185

杨经绥, 许志琴, 宋述光等. 2000. 青海都兰榴辉岩的发现及对中国中央造山带内高压—超高压变质带研究的意义. 地质学报. 74(2), 156-168

张建新, 杨经绥, 许志琴等. 2000. 柴北缘榴辉岩的峰期和退变质年龄:来自u-pb及ar-ar同位素测定的证据. 地球化学. 9(3),217-222.

2017年，被评为中国科学院院士

2014年，杨经绥获中国地质科学院新华联杰出贡献奖

2011年，《青藏高原地体拼合和碰撞造山》项目获国家自然科学二等奖（排名第一）

2011年，被评为美国地质学会会士

2011年，被评为美国矿物学会会士

2010年，《青藏高原地体拼合、碰撞造山及隆升机制》项目获国土资源部科技进步一等奖（排名第一）

2009年，获第十一届李四光地质科学奖

2008年，《大陆深俯冲和科学钻探》项目获国土资源部科技进步一等奖(排名第二)

2008年，获国务院颁发的科学技术事业突出贡献政府特殊津贴

2007年，获何梁何利科技进步奖

2006年，国土资源部“十五”重点科技项目《中国巨型超高压变质带及南北板块汇聚》获国土资源部“国土资源科技技术奖”二等奖(排名第一)

2005年，获国土资源部颁发的“中国大陆科学钻探工程先进工作者”荣誉称号

2003年，获中央组织部、人事部、宣传部、教育部、统战部、科学技术部六部委颁发的《留学回国人员成就奖》

1992年，《昆仑开合构造》项目获地质矿产部科技进步三等奖(排名第二)