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Microspar structures carbonate is characterized by elphent tooth-like structure consisting of fine, equant sparry calcite crystals, and hosting rocks is mainly fine-grained carbonates with mud.

臼齿构造碳酸盐岩是一种具有类似于大象臼齿特征的特殊碳酸盐岩,其微亮晶脉由纯净的、基本等粒的方解石构成,而基质物质则由细粒的、富泥质的灰岩组成。

Microspar structures carbonate is characterized by elphent toothlike structure consisting of fine,equant sparry calcitecrystals,and hosting rocks is mainly finegrained carbonates with mud.

臼齿构造碳酸盐岩是一种具有类似于大象臼齿特征的特殊碳酸盐岩,其微亮晶脉由纯净的、基本等粒的方解石构成,而基质物质则由细粒的、富泥质的灰岩组成。

The correlation analysis indicated that positive correlations existed between electrolyte exosmosis percentage, MDA content and POD activity in both salt and drought treatments, and significant correlations were also found between electrolyte exosmosis percentage, POD activity and MDA content in NaHCO3 stress.

相关分析表明:不论是碳酸盐胁迫还是干旱胁迫,欧李的电解质外渗率、MDA含量和POD活性存在一定程度的正相关,碳酸盐处理下POD活性与电解质外渗率和MDA含量间达到显著的正相关。

The fossiliferous Middle Carboniferous and Permian are well developed in the Deri′angma-Xiala section in the Yunzhug area, Xainza County, northern Tibet.

西藏北部申扎县永珠地区德日昂玛-下拉剖面中石炭系和二叠系地层发育完整,出露良好,化石丰富。该剖面中查果罗玛组碳酸盐岩地层和下拉组碳酸盐岩地层之间的碎屑岩夹灰岩地层,在沉积上表现为冰海相杂砾岩,在古生物化石面貌上表现为特提斯-冈瓦纳古生物群混生。

According to the fossil assemblages and lithology, it is suggested that, during theCretaceous/Paleogene boundary time, Gamba basin was in a warm tropical, subtropicalshallow shelf-circulating environment. It can be recognized as carbonate gentle slope andcarbonate shallow bank facies.

根据岩石薄片鉴别出的生物组合及岩性特征,认为白垩纪/古近纪界线时期,岗巴盆地海洋环境是处于温暖的热带、亚热带浅海陆棚相-开放循环环境中,分为碳酸盐缓坡相和碳酸盐浅滩相。

1Based on the characteristics of carbonatite reservoir in Sangtamu area, we summarize the type of seismic reflection and the distribution of oil and gas.(2)Through the study of the lateral difference of local amplitude, which can predict the short, unorderly reflective energy gobbet of carbonatite reservior, we study the distribution of carbonatite reservoir with crack.(3)Analyzing the change of the seismic waveform, applying nerve network method to classify the seismic waveform, find the rule of its change, recognizing the change rule of seismic facies.(4)Applying the seismic multi-attribute cross method to study the surface and inner of carbonatite reservoir in buried hill. We first extract the 5 kinds of seismic attribute. Through a series of choices, we find those seismic attributes that are sensitive to the change of carbonatite reservoir.

主要的研究包括:①根据桑塔木碳酸盐岩的储层特点,总结了该区的地震反射特征及油气分布特征;②研究出一种有针对性的地震属性--局域振幅横向差异性,来定量刻画潜山内部"短轴"杂乱反射能量团,预测缝洞型碳酸盐岩内部储层的平面分布规律;③通过对地震波形变化的分析,运用神经网络对地震波形进行有效分类,找出波形变化的总体规律,从而认识地震相的变化规律;④应用交会法地震多属性分析方法,对潜山表层和内部分别提取了5大类40种地震属性,通过一系列分析表层及内幕各自优选出3种、4种地震属性用于进行交会分析。

At the stage of platform, the "higher Pb-Zn source bed" would be formed in the plantform-type carbonatite forma tions, especially in the first carbonatite position after every large-scale ingression, by enrichment of weathering deposition, diagenesis, biogenesis and organogenesis.

地台阶段,风化沉积成岩、生物有机质等富集作用形成了地台构造层的碳酸盐建造中(特别是大规模海侵后的第一个碳酸盐岩层位,如D〓、C〓、P〓。)的Pb、Zn上部矿源层。

Especially in carbonate formation, owing to the intricate interstice, the variational size, shape of cave, and the different character of filling, it is almost impossible to get all-around cognition by a single way.

尤其对碳酸盐岩储层来说,由于孔隙空间非常复杂,缝洞的大小、形状、类型、充填物性质的变化很大,用单一的方法全面了解碳酸盐岩储层发育情况几乎是不可能的。

METHODS Therapeutic effects of carbonate buffer mixture (Na2CO3 50 g, NaHCO3 420 g, KCI 20 g, NaCI 100 g, water 10 L) were observed in 120 cases of gastrointestinal atony including forestomach atony, rumen impaction, rumen acidosis, omasum impaction and intestinal constipation.

为进一步验证碳酸盐缓冲合剂对牛胃肠弛缓自然病例的治疗效果,对前胃弛缓(52例)、瘤胃积食(42例)、瘤胃酸中毒(18例)、瓣胃秘结(6例)、肠便秘(2例)等以酸过多性胃肠弛缓为临床特征的120例病牛投服了碳酸盐缓冲合剂(Na 2CO350 g,NaHCO3420 g,KCl 20 g,NaCl 100 g,常水10 L)。

Based on the core, slice observation, geology logging, log and seismic data from more than 15 typical wells, combined with the data of the adjoining area, through macroscopical and microcosmic study and according to the analysis of the kinds and characteristics of the rock components, four types of the sedimentary facies of the study area have been recognized, including Carbonate Platform, Continental-shelf, Slope and Basin. Furthermore, sunken platform, open-shelf and rimmed-shelf have been recognized for the first time.

通过对研究区15余口井岩芯的精细观察,结合薄片鉴定、录井、测井、地震资料及区域沉积资料的分析,应用宏观和微观研究相结合的手段,在岩石结构组分类型及特征分析的基础上,识别并阐述了轮南古隆起奥陶系碳酸盐岩的四种沉积相类型:碳酸盐台地、陆棚、斜坡和盆地,并首次识别出了沉没台地、开阔陆棚和镶边陆棚等相类型。

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