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ultrabasic rock中文是什么意思

  • 超堿巖,超基性巖。

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  • 例句與用法
  • Further imbrication, folding and metasomatism of the ultrabasic rocks occurred at this time .
    超基性巖的進(jìn)一步疊瓦作用,褶曲和交代作用發(fā)生于這個(gè)時(shí)期。
  • The ultrabasic rocks form a complex of large tectonic slices with intercalated slices of sebakwian sedimentary rocks .
    超基性巖與塞巴奎沉積巖巖片相間構(gòu)成一巨大的構(gòu)造巖片的雜巖體。
  • Geochemical features of xiangshan basic - ultrabasic rocks in guangxi , china
    廣西香山巖體地球化學(xué)特征
  • In this thesis , studies show that the xigou ultrabasic rock body is a synthetic ore deposit composed of serpentinite ores , decorative stone ores , metallic and precious metallic ores
    本文實(shí)例(西溝超基性巖體)研究,較系統(tǒng)地查證西溝超基性巖體為一頗具資源潛力的綜合性“礦床” 。
  • The conclusion is that the enrichment of pt , pd is controlled by big and deep fractures , that emeishan basalt is one of the sources of pt and pd , and that basic - ultrabasic rock offers the ore - forming elements and the ore forming energy
    指出研究區(qū)的深大斷裂對(duì)鉑族元素的富集表現(xiàn)出很好的控制作用,峨眉山玄武巖為鉑族元素的礦源層之一,巖漿巖為鉑族元素的富集提供了成礦物質(zhì)及成礦能量。
  • A comparison of the prospecting model of the hf type with the prediction model of the vms type reveals that their thermal dynamic mechanisms are different : the former is related to basic - ultrabasic rock intrusion , while the latter to acidic rock intrusion
    與白銀銅礦區(qū)域地球化學(xué)預(yù)測(cè)模式相比較,富鐵型鉛鋅礦床中除鐵族元素指示基性超基性巖侵入事件外,其他元素均大致相似,兩大類礦床形成的初始熱動(dòng)力條件不同。
  • In this article , model of geological conception in panzhihua - xichang area is established , and then the authors used gis as the tool to analyze the pge ore - forming geological conditions , including geological structure , emeishan basalt , basic - ultrabasic rock and pge geochemical abnormal
    本文在建立攀西地區(qū)鉑族元素礦床地質(zhì)概念模型的基礎(chǔ)上,用地理信息系統(tǒng)( gis )分析了該地區(qū)的鉑族元素成礦地質(zhì)條件,包括地質(zhì)構(gòu)造、峨眉山玄武巖、基性一超基性巖和鉑族元素地球化學(xué)異常特徵。
  • The coqen basin in xizang lies between the bangong - nujiang suture zone and yarlung zangbo suture zone , and once extended northwards and southwards , respectively centred by the qiekan - goicang - asog rift zone as the center of deposition and subsidence during the middle jurassic to the early creatceous . ( 1 ) during the middle - late jurassic , the rift zone was occupied by deep - water turbidites , radiolarian siliceous rocks , shallow - water carbonate rocks , clastic rocks and basic - ultrabasic rocks , while both sides of it by littoral and shallow marine elastic rocks and carbonate rocks
    摘要位于班公湖怒江縫合帶與雅魯藏布江縫合帶之間的措勤盆地,在中侏羅世早白堊世期間具有以且坎古昌阿索裂谷帶為沉積、沉降中心向南北兩側(cè)展開的古地理格局:中晚侏羅世時(shí)期,裂谷帶內(nèi)由深水濁積巖、放射蟲硅質(zhì)巖和淺水碳酸鹽巖、碎屑巖巖片及基性超基性巖等組成;裂谷帶兩側(cè)由濱淺海相碎屑巖和碳酸鹽巖組成。
  • The copper , iron , nickel and silver deposits might be assigned to four metallogenic series : i . the metallogenic subseries of copper , molybdenum , gold , silver deposit related to late devonian - early carboniferous basic - intermediate - acid hypabyssal intrusive - eruptive rocks ; ii . the metallogenic subseriesof iron , copper , zinc deposits related to early carboniferous basic - intermediate - acid volcanic - intrusive rocks ; iii . the metallogenic subseries of copper , silver , iron deposits related to middle - late carboniferous basic - intermediate - acid volcanic - intrusive rocks ; iv . the metallogenic subseries of copper , nickel and platinum group deposits related to late carboniferous - early permian basic - ultrabasic rocks ; 3 , division of regional major metallogenic belts on the basis of the previous work conducted and by following the principles , grounds and methods of the division of metallogenic belts , areas and fields , . in light of this , metallogenic belts of grade iv were divided
    1 、按照成礦系列理論的學(xué)術(shù)指導(dǎo)思想,將研究區(qū)華里西期銅礦床成礦系列劃分為四個(gè)成礦系列亞系列: 、晚泥盆?早石炭世延?xùn)|?土屋?三岔口與中酸性巖漿侵入活動(dòng)有關(guān)的cu 、 mo 、 au礦床成礦亞系列、早石炭世與巖漿作用有關(guān)的鐵、銅、金、銀礦床成礦亞系列、中石炭世與巖漿作用有關(guān)的cu 、 fe 、 ag 、 au礦床成礦亞系列、晚石炭世-早二疊世與幔源基性?超基性巖有關(guān)的銅、鎳、鉑族礦床成礦亞系列并從地層、巖漿巖、控礦構(gòu)造、地球化學(xué)、成礦特征等方面對(duì)各成礦亞系列進(jìn)行了詳細(xì)論述。
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