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1.
《现代地质》1988,2(4):526
N口.D.Palaeozolc >mall,r Foramlnlfera Fauna、on the East Part of 八Orth China Platform… ··’…·’··’”……··””·’”……’……·”…··”’…………………………··Zheng hong(19)Tge Character5of Sllurlan Rugose Corals and the Discuss】on about the Age of tile Strata of Qujlnz Reg。on.Yu。nan··,,……·,··,,……,·,………,…··,··,…,…Dlnrr Chunmine(22〕sell—e口tarV rades and Te口tono—paleogeographv of the Late sin二an nengving ror回口ation In yor。bwest。rn Hubel…  相似文献   

2.
Planning of protection of geological environment FANG Jian- hua  XIE Jun- cheng  QIAO Guo- chao et al.(1— 1)………The harm ,inducing factor and prevention counterm easures of geological hazards in Jiangsu GAO De- yun(1— 8)…………The city disaster charecteristics and disaster reduction counterm easure in UrumqiMaihepireti· WU L AMU  Annigen er MOMING(1— 12 )…………………………………………………………………Reviews and evaluation of the geological envirom ent of Hebei provi…  相似文献   

3.
<正>We thank Tan Mingxuan et al.(2017)for their comments stimulated by our short paper in the recent Acta Geologica Sinica(English edition).We are grateful for the opportunity to expand on the model of the supercritical hyperpycnal flow deposits in the Beilaishi section on the Lingshan Island,and to explain why the model proposed by Tan Mingxuan et al.(2017)cannot explain the bulk of  相似文献   

4.
Sedimentary Suites(SDS)of Early St。la。P。nod in China………··、………M。ng Xiangkua。t al·(14).Meucd and ExamPles of Making maPs of World Reconstruu】onby a MlctocO*Puter·-·’··’··’·’…… ,……,……….、…………………………………………………··。,……··Li Xiang andZbang Lingkua(ZP)Geographic posit。on of the Qaidam Bio。k in L。ie Carboniferou。…·。…………·Li Yanpingetal.(32)Ontozenv of Homalophyllum Simpson,1900 and A SEM Study of itsMlcros发eletal 〕true…  相似文献   

5.
No.1Petrographic Studie。of The Volcanic Complex in The Xiang。han Caldera …………·……………………………………………………………”Pang Xiheng,ttou Wenyao,Wan Guoliang(10)charactcristic.of The Skarn Zoning of The Makeng and Yeng。han Iron Ore Deposits in Fujian and Thier Relationship with’the Mineralization Zoning………………Zhao Yining,Tan Huifing,Sun Jinghua(22)Mossbauer Study of Bafertisite……·………………··Wu Gongbao,Wang Toutong,Zhang Shuiun,Ding Haohua(29)The Disc…  相似文献   

6.
正1 Introduction Cold environments on the planet occur in the Antarctic,the Arctic and high mountains which cover with ice and snow permanently.Microorganism adapted to cold habitats has been detected,but most of them were prokaryotes.(Morgan-Kiss et al,2006;jungbut et al,2012).Research on cold-adapted microorganism has  相似文献   

7.
ECONOMIC GEOLOGY     
P .10一18,26 ref) Aceording ro researeh on teetonie basinformation and post一reetonle deformarion ofthe Devonian sedinlenrary,the georhermalevents of teeronie一l:ydrorhermal fluid In the1〕evonian hydrothermal dePosition basins inthe Qlnling orogen ean be reeognized.In rheeoarse of sedlmentary basin formation andevolution,geothermal regime一5 variable in thebasin but still ean be reeovered on the basis ofspee一al approaeh·In the reeovery of geother-mal srare and geothermal evolution in the …  相似文献   

8.
Trace elements in cassiterite,including Ta,W,Fe,Mn,Ti,Zr,V,Sc,Si,Al,In,Ga,Ge,Be,Bi,Ag,Sb,As,Cu,Pb,Zn,Co and REE,have been studied by many workers (Shan Zhenhua etal.,1998;Huang Zhou Tianren et al.,1987;Wu Qingsheng et al.,1988;Hu Zening,1988,Li Zhong-qing 1988 Mingzhei et al.,1988;Wang Lihua et al.,1988;Liu Kanghuai,1990).Up to now,however,most of the previous studies are concerned with trace-element variations in cassiterites of different occurrences and colors from different types of ore deposits,Data concerning the modes of occurrence of these trace elements are rare,except for the contention that Nb-Ta,Fe^2 -Mn-Fe^3 and W-Fe^3 may substitute isomorphously for Sn as pointed out by Zhou Tianren et al.(1987) and Moller et al.(1988).In this paper we are concerned with the compositional characteristics as well as the modes of occurrence of trace elements in cassiterites from quartz veins and greisens in the Dupangling tin field,Guangxi,based on multivariate statistical analyses.Tin mineralization in the Dupangling area is found associated with the medium-to fine-grained protolithionite-albite granite(γ5^2b) and its outer contacts.Cassiterite occurs,with wolframite,both in quartz veins in the contact and in greisens within the granite.^1) Spatially,greisens become dominant over quartz veins in the contact andin greisens with the granite.^1)Spatialy,gresens become dominant over quartz veins in going from the contact to the interior of the granite and with increasing depth.The greisens are of various shapes.The vein-shaped and the sheet-shaped greisens at the top of the granie are rich in quartz and the chambered greiens always constitute rich ores and contain abundant topaz or mica.Genetically,Sn,W mineralizations associated with the protolithionite-albite granite(γ5^2b) are considered to have been formed from fluid melt derived from the ore-forming magma responsible for the granite(γ5^2b).  相似文献   

9.
COMMENTARY A preliminary discussion on the metallogenesis and the exploration access of the large deposits in Xinjiang………CHEN Zhe-fu (1-6) A preliminary discussion on the metallogenesis and the exploration access of suprelarge deposits in Xinjiang……CHEN Zhe-fu (2-87) Industrial situation of gold and development antidote in China………………………………………………………WANG Qin (2-90) Resource types and development prospect of ornamental stones in Xinjiang……………………LIU …  相似文献   

10.
1. IntroductionThe discovery of the ophiolites (composed of mafic-ultramafics plutons, radiolarian silicalites and the basic metavolcanic rocks) in Mianlue zone was one of the most important progresses in the study on Qingling orogen in recent years (Zhang G W et al., 1995, 1996; Zhang Z Q et al., 1996; Yin et al., 1998; Lai, 1997; Lai et al., 1996; Meng et al., 1999). Many geologists got the conclusions as followings. (1) along the Mianlue zone, the oceanic crust developed in late Paleoz…  相似文献   

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