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测试师资

教学与科研成果

研究兴趣

1.西南印度洋脊深海橄榄岩岩石成因

2。西南印度洋深部地幔物质组成与演化过程

3.藏东南新生代后碰撞岩浆活动与斑岩成矿作用

 

研究成果

[1].Shen Y,Zheng Y C*,Hou Z Q,Huizenga J M,Zhang A P,Wang Z X,Li X,Xu P Y,Wu C D,Liu S Q.Pre-Late Eocene position of the Lüchun-Jinping micro-terrane in western Yangtze Craton:Constraints from Eocene-Oligocene lamprophyres in southeastern Tibet.Lithos,2022,414-415:106622.https://doi.org/10.1016/j.lithos.2022.106622.

[2].Liu SQ,Zheng Y C*,Hou Z Q,Shen Y.Multi-stage crustal magma reservoirs of ultrapotassic rocks recorded by zoned clinopyroxene.Journal of Asian Earth Sciences,2022,226:105072.https://doi.org/10.1016/j.jseaes.2021.105072

[3].Wu CD,Zheng YC*,Hou ZQ,Xu PY,Zhang LY,Shen Y,Wang L,Li X.Petrogenesis of Eocene Wangdui adakitic pluton in the western Gangdese belt,southern Tibet:Implications for crustal thickening.Geological Magazine,2022.

https://doi.org/10.1017/S0016756822000206

[4].Shen Y,Zheng Y C*,Hou Z Q,Zhang A P,Huizenga J M,Wang Z X,Wang L.Petrology of the Machangqing Complex in Southeastern Tibet:Implications for the Genesis of Potassium-rich in Adakite-like Intrusions in Collisional Zones.Journal of Petrology,2021,62(11):egab066.https://doi.org/10.1093/petrology/egab066

[5].Zheng Y C*,Shen Y,Wang L,Griffin W L,Hou Z Q.Collision-related porphyry Cu deposits formed by input of ultrapotassic melts into the sulfide-rich lower crust.Terra Nova,2021,33:582-589.

[6].Wang Z X,Zheng Y C*,Xu B,Hou Z Q,Zhang A P,Shen Y,Ma R,Wu C D,Xu P Y.Hydrous juvenile lower crust at the western Yangtze Craton margin as the main source of the Beiya porphyry-skarn Au deposit.Acta Geologica Sinica (English Edition),2021.https://doi.org/10.1111/1755-6724.14788

[7].Liu S Q,Zheng Y C*,Shen Y,Hou Z Q,Wang L,Wang Z X.Source of the ore-forming adakitic porphyry at the Beiya super-large Au deposit,western Yangtze Craton:New evidence from zircon U-Pb ages of the amphibolite xenoliths.Acta Geologica Sinica (English Edition),2020,94:208-209.

[8].Xu P Y,Zheng Y C*,Yang Z S,Hou Z Q,Shen Y,Wang Z X,Wu C D,Zhou L M.2020.Metallogeny of the continental collision-related Jiagang W-Mo deposit,Tibet:Evidence from Geochronology and Petrogenesis.Ore Geology Reviews,122:103519.

[9].Zhang A P,Zheng Y C*,Xu B,Fu Q,Ma W,Wu C D,Zhang C,Shen Y,Fei F.Metallogeny of the Lietinggang-Leqingla Fe–Cu–(Mo)–Pb–Zn polymetallic deposit,evidence from Geochronology,Petrogenesis,and Magmatic oxidation state,Lhasa terrane.Ore Geology Reviews,2019,106:318–339.

[10].沈阳,郑远川*,张爱萍,王梓轩,王璐,徐培言,吴昌炟.滇西剑川始新世富碱岩浆岩锆石U-Pb年代学与Sr-Nd-Hf同位素地球化学及其对岩石成因的制约.岩石学报,2019,35(3):849-866.

[11].罗晨皓,周晔,沈阳.云南姚安Au-Pb-Ag矿床含矿富碱岩浆岩地球化学特征及岩石成因.地球科学,2019,44(6):2063-2083.

[12].徐培言,郑远川*,杨竹森,沈阳,马睿,王梓轩,吴昌炟.西藏甲岗雪山钨钼矿床成矿流体及成矿物质来源.地球科学,2019,44(6):1974-1986.

[13].沈阳,郑远川*,马睿,张爱萍,徐培言,吴昌炟,王梓轩.云南马厂箐铜钼矿成矿岩体的角闪石和黑云母矿物学特征及其意义.矿床地质,2018,37(4):797-815.

[14].周晔,沈阳,侯增谦*,谢鑫,罗晨皓.滇西六合正长斑岩中角闪石、黑云母和锆石的特征及其指示意义.岩石矿物学杂志,2018,37(4):547-561.

[15].徐培言,郑远川*,付强,杨竹森,沈阳,马睿,王梓轩,吴昌炟.西藏首例云英岩型钨矿—甲岗雪山W-Mo多金属矿床地质特征研究.岩石矿物学杂志,2017,36:227-240.

 

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