1) authigenic carbonates
自生碳酸盐岩
1.
The authors report on the mineralogical features and carbon-oxygen isotope composition of the authigenic carbonates build-up of Samples TVG-1 and TVG-11 from Jiulong methane reef in the South China Sea.
碳氧同位素和矿物的显微结构特征都说明九龙甲烷礁碳酸盐岩是烃类渗漏微生物作用而形成的自生碳酸盐岩,可能是天然气水合物分解引起的沉积,显示该区存在水合物的可能性很大。
2) methane seep carbonate
甲烷冷泉自生碳酸盐岩
3) Authigenic Carbonate
自生碳酸盐
1.
Authigenic Carbonate Oxygen and Carbon Isotope in Angulinao Lake and Environment;
安固里淖自生碳酸盐碳氧同位素组成与环境
2.
C-O isotope composition of the authigenic carbonate in Low Tertiary reservoir sandstones in Tarim Basin and its implication on the fluid origin.;
塔里木盆地下第三系储层砂岩自生碳酸盐碳氧同位素组成及流体来源讨论
3.
Sedimentary carbonate consists mainly of allochthonous carbonates produced by surface runoff and authigenic carbonates produced by inorganic precipitation.
沉积物碳酸盐包括物源区带来的外源碳酸盐和湖泊内生沉淀产生的自生碳酸盐,其中只有自生碳酸盐才具有古气候指示意义。
4) growth rate of carbonates
碳酸盐岩生长率
1.
First of all,the development potentials of the two types of reservoirs mentioned above are defined according to the growth rate of carbonates,then the distribution of intra-sequence reservoirs is predicted through detailed delineation of the distribution of isochronous unit reef flat facies;and the development of sequence boundary reservoirs is predicted on the basis of.
在研究中首先根据碳酸盐岩生长率判断上述两类储层的发育潜力;然后,通过等时单元礁滩相展布的精细刻划预测层序内部储层的发育分布,通过层序不整合面类型及性质分析,预测评价层序界面储层的发育状况。
5) hydrocarbon generation of carbonate
碳酸盐岩生烃
6) Oil generation of carbonate rocks
碳酸盐岩生油
补充资料：长白山冷泉
长白山冷泉，晶莹甘芳，和山区的温泉一样，遍及整个林海，好似一颗颗璀璨的明珠，镶嵌在深山林海之中。其中长白药水泉是旅游区最著名的冷泉。
它位于头道白河西岸，距二道河火车站17公里。药水泉有5个出水口，水温常年保持在8℃左右。盛夏时节来到这里，喝上几口泉水，感受又麻又辣，所以有“天然汽水”的美称。药水泉内含锶、锂等元素，这种矿泉水目前在世界上比较受欢迎。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条