carbonate mineral造句

• The characteristic frequencies of the raman and infrared spectra of the fergusonite and aeschynite group minerals, monazites and the rare earth fluoro-carbonate minerals have been determined and assigned
  (3)变生态矿物拉曼光谱的强度很弱、谱线宽而弥散，而退火晶态矿物的拉曼谱峰强而尖锐。
• When diapir fractures opened, entering of hot fluid into reservoirs may cause dissolution of carbonate minerals, and when diapir fractures closed, carbonate minerals precipitated in high temperature condition
  底辟断裂开启时，深部富c02热流体进入储层，导致碳酸盐矿物溶解；通道闭合时，高温使碳酸盐矿物沉淀。
• When diapir fractures opened, entering of hot fluid into reservoirs may cause dissolution of carbonate minerals, and when diapir fractures closed, carbonate minerals precipitated in high temperature condition
  底辟断裂开启时，深部富c02热流体进入储层，导致碳酸盐矿物溶解；通道闭合时，高温使碳酸盐矿物沉淀。
• Among the discrimination criterion controlling the alteration of carbonate, neither cathodoluminescence of the carbonate minerals nor t he content of sr can act solely as discrimination criterion for controlling the alteration of marine carbonate
  在碳酸盐的阴极发光性、sr含量和mnsr比值三个判断成岩蚀变性的标准中，阴极发光性和sr含量不能单独作为判断标准来检测海相碳酸盐矿物的成岩蚀变性。
• With the intermittent activity of hot fluid containing cc ^, ferrous carbonate minerals dissolved and precipitate repeatedly many times . in addition, dissolution of shells and feldspars, decrease of chlorite and increase of kaolinite could be found
  随着富co_2热流体多次间歇性入侵导致了含铁碳酸盐矿物的反复多次溶解和沉淀、生物介壳大量溶蚀和长石铸模孔的形成以及绿泥石消失、高岭石增加等。
• On the contrary, the reservoirs that were not influenced by hot fluid just were in early diagenetic stage b . 2 . based on the synthetic analysis of varied data, the mechanism of repeated dissolution and precipitation of ferrous carbonate minerals has been discussed
  在进行充分的岩石学研究基础上，利用电子探针、稳定同位素及包裹体分析数据，探讨了异常成岩演化储层中含铁碳酸盐矿物反复溶解和沉淀的机理。
• The gangue minerals are mostly carbonating minerals, fluorite, barite, celestite and so on; the rock alteration is slightly silicified, carbonated, baritizated, celestited, which is low-temperature alteration . because of continual downgoing extrusion from india plate to euro-asian plate, there are some thrusting nappe structures in lanping basin related to the orogens on the two sides
  矿床中矿石矿物发育典型的中低温热液成因的矿物组合，如黝铜矿系列、方铅矿、黄铜矿等，脉石矿物主要为碳酸盐类矿物、萤石、重晶石、天青石等；围岩蚀变主要发育弱硅化、碳酸盐化、重晶石化、天青石化等低温蚀变组合。