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1.In Zhongtiao Mountains , the main strata are Archean Shushui Complex(granulite facies complex), Jiangxian Group (amphibo-greenschist facies metamorphic rock), Paleoproterozoic Zhongtiao Group (metamorphic conglomerate and quartzite), middle Proterozoic Xiyanghe Group(andesite and sedimentary rock), Neoproterozoic Changcheng group(sedimentary rock).
中条山地区出露的地层主要有新太古界涑水麻粒岩 -角闪岩相杂岩、绛县群角闪 -绿片岩岩相变质岩、古元古界中条群绿片岩相变质岩、担山石群变质砾岩 -石英岩、西阳河群安山岩、沉积岩和中新元古界沉积岩。收藏指正
2.The seismic sequence frame and seismic facies in Darfur Group of eastern sag,Nugara Depression,Muglad Basin
Muglad盆地Nugara坳陷东凹Darfur群地震层序格架和地震相收藏指正
3.The Application of Markov Chain’s Analysis in Studying Sedimentary Facies of Dongzakou Group of Later Carboniferous Epoch in Lixian County, Gansu Province
马尔柯夫链分析在甘肃礼县地区上石炭统东扎口组沉积相研究中的应用收藏指正
4.Their appearence, optical character, components and textures all vary reich metamorphic temperatures and pressures, showing the existence of the progressive metamorphic zone (low greenschist facies-high greenschist facies-low amphibole facies)of the Kuanping Group from the south to the north or the distribution of the regional heat flow.
其形态、光性及成分、结构随变质温度和压力的变化,显示宽坪群自南向北前进变质带(低绿片岩相—高绿片岩相—低角闪岩相)的存在或区域热流的分布状况。收藏指正
5.THE STORM DEPOSITS AND CHANNEL FACIES IN GUANSHAN FORMATION, WUTONG GROUP FROM SOUTH JIANGSUAND EAST ANHUI
苏南皖东五通群观山组的近岸风暴沉积与湖道沉积收藏指正
6.STUDY ON MICRO-FACIES OF Es_3~4 Ⅱ SAND GROUP IN THE SANCHUNJI AREA
三春集地区Es_3~4Ⅱ砂组沉积微相研究收藏指正
7.THE CHARACTERISTICS OF SEDIMENTARY SYSTEM-CONTINENTAL FACIES VOLCANO IN LATER CARBONIFEROUS BATAMAYI GROUP,ZHI-FANG REGION,EAST JUNGGER
东准噶尔纸房地区晚石炭世巴塔玛依内山组陆相火山-沉积体系特征收藏指正
8.The CALEDONIAN METAMORPHISM AND METAMORPHIC FACIES SERIES DIVISION OF MIDDLE PROTEROZOIC GROUP STRATA IN NORTH WEST OF FUJIAN PROVINCE
闽西北中元古界地层加里东变质作用和变质相系划分收藏指正
9.Analyses and researches systematically the facies and depositional environment of Miocene Epoch Wudaoliang Group in Hoh Xil basin in hinterland of the Tibet Plateau .
论文重点对青藏高原腹地中新世五道梁群和唢呐湖组的岩相和沉积环境进行了系统分析和研究。收藏指正
10.The Wulashan gold-bearing ore veins are located in late Archean Wulashan group high grade metamorphic area (mainly at amphibolite facies, even to granulite facies),and controled by Wulashan fault structure zone.
乌拉山含金矿脉赋存于晚太古界乌拉山群高级变质岩区（变质程度以角闪岩相为主，可达麻粒岩相），受控于乌拉山断裂构造带。收藏指正
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