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hypabyssal intrusive meaning in Chinese

浅成侵入体

Examples

  1. By physiognomy feature , it could be divided into three types of thermal structure : positive dome model , negative collapse model and border dome core collapse model . based on the depth degree or magma - thermal influenced , it could be divided into five types of thermal structure : ( ancient ) geothermal anomaly focus region model , superficial volcano eruption hydro - thermalism and hypabyssal intrusive model , thermal anticline ( thermal dome ) model , mid - deep intrusive model , deep mantle ( crust ) thermal plume model ; and put forward a perfect model of the thermal structure . there are many interaction system could be induced into a systematic thermal interaction , include : ocean - continent system , basin - mountain interaction , superficial and mid - deep crust - mantle interaction , crust - mantle commingle interaction , vertical thermal interaction ( delamination ) etc .
    依据地貌形态分为三类:正向穹窿型、负向塌陷型、边隆核陷型:依据岩浆-热力作用影响的深浅程度或深度分为五类: (古)地热异常群集区、表浅层火山喷发-热液活动与浅成侵入型、热力背斜(热穹窿) 、中深层侵入型、深部地幔(地壳)热柱型;提出了热力构造作用空间分布的理想模式,将洋陆系统、盆山作用、浅表与中深部壳幔作用、壳幔混合、垂向热力作用(拆沉)等纳入一个整体统一的热力作用系统中,为盆地动力学研究打开了一个新窗口;研讨了热力构造研究方法。
  2. 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 、按照成矿系列理论的学术指导思想,将研究区华里西期铜矿床成矿系列划分为四个成矿系列亚系列: 、晚泥盆?早石炭世延东?土屋?三岔口与中酸性岩浆侵入活动有关的cu 、 mo 、 au矿床成矿亚系列、早石炭世与岩浆作用有关的铁、铜、金、银矿床成矿亚系列、中石炭世与岩浆作用有关的cu 、 fe 、 ag 、 au矿床成矿亚系列、晚石炭世-早二叠世与幔源基性?超基性岩有关的铜、镍、铂族矿床成矿亚系列并从地层、岩浆岩、控矿构造、地球化学、成矿特征等方面对各成矿亚系列进行了详细论述。
  3. There are two stages to crux maifan stone ' s formation , the first stage is the forming stage of primary material , that is to say , the stage of mother rock formation , in this stage , the latter hypabyssal intrusive of crystallization fractionation and self - metamorphic process are an important factor to make sure them have many trace elements
    麦饭石的形成中有两个阶段是十分关键的,第一个阶段是基本物质的形成阶段,即母岩的形成阶段。在这一阶段中岩浆分异结晶晚期的浅成侵入以及自变质作用,是保证其富含营养微量元素的重要条件。

Related Words

  1. hypabyssal
  2. hypabyssal rock
  3. hypabyssal rocks
  4. hypabyssal instrusive
  5. intermediate hypabyssal sill
  6. intrusive
  7. intrusive monitoring
  8. no intrusive
  9. intrusive force
  10. intrusive dike
  11. hypabyssal
  12. hypabyssal instrusive
  13. hypabyssal rock
  14. hypabyssal rocks
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