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1)  hydrocarbon generation of carbonate
碳酸盐岩生烃
2)  marine carbonate source rocks
碳酸盐岩烃源岩
1.
In order to evaluate the marine carbonate source rocks objectively and determine the exploration direction, it is necessary to develop new method and set up a new identification and evaluation .
我国海相碳酸盐岩烃源岩的特点是有机质丰度低、热成熟度高、经历的地质历史较长、研究难度大。
3)  carbonate source rock
碳酸盐烃源岩
1.
Based on the investigations of carbonate source rocks, which had expelled oil and gas in the past, and studies of simulation experiments about the generating and expelling hydrocarbons in carbonate rock at a series of temperature and pressure conditions.
通过典型碳酸盐型油气田的野外调查研究和对未成熟碳酸盐生油岩在外加温、外加压条件下所作的生烃一排烃模拟实验结果,获得下列新的认识:(1)碳酸盐烃源岩排烃的驱动力主要不是来自地层的压实作用,而是由于生烃过程中分子体积膨胀所产生的内应力(即生烃增压)。
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)  Oil generation of carbonate rocks
碳酸盐岩生油
6)  microbial carbonate
微生物碳酸盐岩
1.
As a main category of microbial carbonates,the thrombolite together with the oncolite is grouped into "microphytolites" and is used parallel to the stromatolite,whereas,thrombolites is still called catagraphites.
作为微生物碳酸盐岩的主要类型,凝块石与核形石曾经被统称为"微植石"而与"叠层石"平行使用;但是,鉴于叠层石也具有凝块状组构,所以凝块石又被译作"斑粒石",或被称作"花纹石",因此,凝块石这一概念还显得有些混乱。
补充资料:烃基二硫代碳酸盐
分子式:
CAS号:

性质:它是目前应用最广泛的硫化矿捕收剂,因呈黄色,故称黄药。黄药的化学名称是烃基黄原酸盐或烃基二硫代碳酸盐,通式中Me为钠或钾,也有制成铵盐的,R为不同的烷基、烷芳基、环烷基、烷氧基等。黄药的品种很多,常用的有乙基黄药、丁基黄药、异丙基黄药、异丁基黄药、戊基黄药、己基黄药等。黄药的分子结构与浮选性能有密切关系,一般而言,黄药分子中的碳链越长,其捕收能力越强,即随着醇基分子量的增加而增大;带有支链的同系异构体较直链的捕收作用强。 

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