岩溶作用的英文

• karstification

• "岩溶"英文翻译    karst
• "作用"英文翻译    act on; affect
• "岩溶作用带" 英文翻译 :    karstification zone
• "补体溶作用" 英文翻译 :    complement hemolysis
• "出溶作用" 英文翻译 :    exsolution
• "冻溶作用" 英文翻译 :    freeze-and-thaw action
• "共加溶作用" 英文翻译 :    cosolubilization
• "过溶作用" 英文翻译 :    transfusion
• "加溶作用" 英文翻译 :    solubilization
• "胶溶作用" 英文翻译 :    peptidization; solation
• "离溶；出溶作用" 英文翻译 :    exsolution
• "离溶作用" 英文翻译 :    exsolution
• "粒溶作用" 英文翻译 :    crinophagy
• "淋溶作用" 英文翻译 :    eluviation
• "淋溶作用层" 英文翻译 :    zone of eluviation; zoneofeluviation
• "深溶作用" 英文翻译 :    anatexis
• "渗溶作用" 英文翻译 :    leaching
• "压溶作用" 英文翻译 :    pressure solution
• "异溶作用" 英文翻译 :    heterolysis
• "再增溶作用" 英文翻译 :    resolubilization
• "增溶作用" 英文翻译 :    solubilization
• "自溶作用" 英文翻译 :    autodigestion; autolysis
• "自溶作用；自消作用；回溶作用" 英文翻译 :    autolysis
• "固态脱溶作用" 英文翻译 :    solid state precipitation
• "化学淋溶作用" 英文翻译 :    chemical eluviation

• Except the simmering in deep area , other three kinds of hydrothermal karst would associate and induce geological disasters
  除深部相浸煮蚀变作用外，其余3种热水岩溶作用都可伴生和引起地质灾害。
• This research demonstrates that this area is suitable for the development of large scale weathering crust and karstic reservoirs
  结果表明，研究区域适宜大规模风化壳岩溶作用的发生以及岩溶型储层的发育。
• It was considered that karstification is the base of reservior formation , and lithology and faulting control the formation and development of internal reservior
  其发育规律为：岩溶作用是下古生界储集层发育的基础；岩性和断裂作用决定内幕储层的形成与发育。
• The occurrence of the palaeokarstification is closely associated with the sequence boundaries and lowstand systems tract created by the guizhou - guangxi , ziyun and dongwu movements
  古岩溶作用的发生与黔桂运动、紫云运动、东吴运动等所形成的层序界面和低位体系域密切。
• The integration of well logs , outcrops and tectonic data shows that the youjiang basin underwent several stages of palaeokarstification during the late palaeozoic
  摘要钻井、露头和区域构造资料的分析结果表明，晚古生代的右江盆地存在多期次的岩溶作用，通常具有1 ~ 3个岩溶旋回。
• One to three karst cycles may be recognized mostly at the top of the upper permian strata , top of the middle permian maokouan strata and top of the carboniferous strata and subordinately at the top of the devonian strata
  这些古岩溶作用主要存在于上二叠统顶部、中二叠统茅口组顶部和石炭系顶部，其次是泥盆系的顶部。
• Owing to the difference of co2 concentration and hydro - chemical characteristics at different altitudes , the karst processes in the foot part is stronger than those in the top of the jinfo mountain
  岩溶动力系统主要表现为：土壤co2和水化学特征的差异显著，从而形成了山上山下两个不同特征的岩溶动力系统，山下岩溶作用明显强于山顶。
• The genetic types include weathering , regional meteoric corrosion , regional dolomitization regional paleokarstification , regional dedolomitization and regional fresh - water cementation and filling
  研究区存在包括风化、区域性大气淡水溶蚀、区域性白云岩化、区域性古岩溶、区域性去白云岩化和区域性淡水胶结充填等6种岩溶作用的层序成因类型。
• In this research , some conclusions are followed : l ) in the tahe oilfield , multiphase tectonic movement and pleokarst were so deeply worked on the diagenesis that the types of diagenesis are various , and the relation of those are complicated
  本次研究最终得出如下结论： 1 )研究区由于受到多期构造运动的影响，又受到多期古岩溶作用的叠加改造，成岩作用类型多样，关系复杂。
• Huge deep fractures in the east of china have a little influence on the pore of carbonatite reservoir of ? - o stratum in the regions of zhuangxi and chengdao . the karstification which probably happened at xishan tectogenesis period is also very limited
  我国东部深大断裂对桩西、埋岛地区寒武一奥陶系碳酸盐岩的储层孔隙影响很小，可能发生在喜山期的岩溶作用(深部流体带来的岩溶作用)也是十分有限的。