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．