1) dolomitization
[英][,dɔləmitə'zeiʃən] [美][,dɑləmətə'zeʃən]
白云石化
1.
Fluid origin of burial dolomitization and hydrocarbon accumulation model of backward charging in Changxing formation, NE Sichuan basin
川东北长兴组埋藏白云石化流体来源与油气倒灌式成藏
2.
Grain dolostone is formed in the deep burial dolomitic environment by mixing-water dolomitization.
礁白云岩具有典型的混合带白云石化特点,受海平面频繁变化影响;颗粒白云岩的形成与混合水白云石化作用和深埋藏成岩作用有关;准同生白云石化或卤水回流渗透白云石化是泥晶-微晶白云岩(含膏云岩)的形成机制。
3.
These characteristics reflect that dolomitization occurred in synsedimentary heavy brine environme.
这些特征反映了白云石化作用发生在准同生超浓缩卤水条件下,古盐度为36。
2) dolomization
白云石化
1.
Results The conclusions are the favorable original facies belt,the degree and types of dolomization,karstification in deep depth,fracturing and its associated fractures are the keys to the development of the reservoir.
结果有利的原始沉积相带、白云石化作用的程度与类型、深埋岩溶作用、断裂作用及其伴生裂缝是储层发育的关键。
3) dedolomitization
[,dedəlɔmitai'eiʃən]
脱白云石化
4) dolomitize
[英]['dɔləmitaiz] [美]['dɑləmə,taɪz]
化成白云石
5) dolomitization
[英][,dɔləmitə'zeiʃən] [美][,dɑləmətə'zeʃən]
白云石化作用
1.
The present paper suggests that karstification and dolomitization are the most important formation mechanisms of the Lower Paleozoic carbonate reservoir rocks in Jiyang Depression,depending on the study of the trace elements(Mn,Sr) and stable isotope(O,C,Sr).
通过对济阳坳陷下古生界碳酸盐岩的锰、锶等微量元素及氧、碳、锶等同位素的测试与分析研究,认为岩溶作用和白云石化作用是济阳坳陷下古生界碳酸盐岩储层形成最为重要的成因机理。
2.
Nowadays,the progress of research about dolomitization and the issue of dolostone has been acquired.
近年来,关于白云石化作用及白云岩问题,取得了更深层次的发展。
3.
By analyzing the accessory element such as Mn, Sr, Mg, etc, and isotope such as ~ 13 C, ~ 18 O, ~ 87 Sr/~ 86 Sr etc, the authors consider that the most important mechanism of the carbonate reservoir of Lower Paleozoic are dolomitization and karstification.
通过对桩海地区下古生界碳酸盐岩的锰、锶、镁等微量元素及氧、碳、锶等同位素的测试与分析研究认为,白云石化作用和岩溶作用是济阳坳陷桩海地区下古生界碳酸盐岩潜山储层最为重要的成因机制。
6) dedolomitization
[,dedəlɔmitai'eiʃən]
去白云石化反应
1.
Results showed that the dedolomitization of dolomitic rock takes place in situ.
结果表明 ,白云岩中的去白云石化反应属原位化学反应 ,反应仅限定在界面处集料边缘反应环的窄小区间内 ,反应生成的胶体尺寸的水镁石吸附 OH-离子形成带负电的扩散双电层 ,阻止 OH-离子向白云岩内部迁移 ,水镁石和方解石在有限空间成核与生长 ,形成无序排列的水镁石和方解石晶
补充资料：白云石,白云岩,石灰岩
CAS：1317-65-3
中文名称：石灰石；电石灰岩；石灰石粉；霰石,文石；方解石,碳酸钙晶体；碳酸钙,白垩；白云石,白云岩,石灰岩；石灰石,石灰石；大理石,大理岩,云石,玻璃球；波特兰石；白垩,磨细白垩粉,白垩粉
英文名称：Limestone；Agstone；agricultural limestone；aragonite；atomite；bell mine pulverized limestone；calcite；calcium carbonate；carbonic acid, calcium salt；chalk；dolomite；domolite；franklin；lithograpic stone；marble；natural calcium carbonate；portland stone；sohnhofen stone；whiting；limestone,powder；flux lime
中文名称：石灰石；电石灰岩；石灰石粉；霰石,文石；方解石,碳酸钙晶体；碳酸钙,白垩；白云石,白云岩,石灰岩；石灰石,石灰石；大理石,大理岩,云石,玻璃球；波特兰石；白垩,磨细白垩粉,白垩粉
英文名称：Limestone；Agstone；agricultural limestone；aragonite；atomite；bell mine pulverized limestone；calcite；calcium carbonate；carbonic acid, calcium salt；chalk；dolomite；domolite；franklin；lithograpic stone；marble；natural calcium carbonate；portland stone；sohnhofen stone；whiting；limestone,powder；flux lime
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参考词条