洼

However, 35％ of the Chinese-Holstein milk samples failed to coagulate.

用放射免疫法测定了全奶麦洼牦牛和半奶麦洼牦牛血浆中的激素含量。

From geometry and forming mechanism, five secondary styles of the extensional-type structural style, including tilted faulted-block, slide faulted-ramp, buried hill draping, gravitative antiform and diapir, were reported.

滑动断阶构主要发育在坳陷的陡坡带，底辟构造常见于坳陷的洼陷带，潜山披覆构造多发育在盆地四周隆起区与洼陷中的潜山带，而重力背形构造大多发育在主断层的下降盘。

It was the first time the sequence stratigraphy study had been done all across Naimanqi Depression. Jiufotang Formation of Naimanqi Depression was divided into two third-class sequences (SQ1 and SQ2) and five system tracts (SQ1 has LST, TST and HST; SQ2 has TST and HST), and in High System Tract of SQ2, two fourth-class sequences were defined (Ssq1 and Ssq2).2. According to the analysis of core and logging data, we considered that it is the delta fan facies and established the electrofacies model.3. The distribution of reservoir sand bodies had been predicted in the areas without well data by combining the methods of sequence stratigraphy and reservoir inversion. In addition, we summarized the method and process of combining geology and geophysics to predict reservoirs and we made a good prediction by applying it.4. Combining with sequence and depositional types, sandstone thicknesses and reservoir properties, based on Petrel Software platform, we used fuzzy mathematics to comprehensively evaluate reservoirs and define favorable areas. We classified the reservoirs in Naimanqi Depression into five types (TypeⅠ, TypeⅡ, TypeⅢ, TypeⅣand TypeⅤ) and pointed out four favorable areas: Block Nai 1, Block of western Naican 1-Zhangjia Depression, Block Nai 6 and Block of Xinfa-Zhangjia Depression.

其主要创新点如下：1、首次在整个奈曼旗凹陷范围内进行了层序地层学的研究，将奈曼旗凹陷九佛堂组地层分为2个三级层序(SQ1和SQ2)和5个体系域(SQ1由LST、TST和HST组成，SQ2由TST和HST组成)，并在SQ2的高位体系域中又识别出两个四级层序(Ssq1和Ssq2)。2、根据岩芯分析和测井资料识别，定义了研究区扇三角洲沉积相类型，并建立了测井相模板。3、通过层序地层学的研究，结合储层反演，对奈曼旗凹陷层序格架内没有井的区域进行了储层砂体的空间展布预测，并总结了地质-地球物理综合储层预测的方法与思路流程，在应用中取得了良好的预测效果。4、结合层序、沉积类型、砂岩厚度和储层物性等方面，以Petrel软件为基础平台，利用模糊数学的方法进行储层综合评价及有利区划分，将奈曼旗凹陷储层划分为五个级别(Ⅰ类、Ⅱ类、Ⅲ类、Ⅳ类和Ⅴ类)，并预测了四个有利区块，分别为：奈1区块、奈参1西-张家洼子区块、奈6区块和新发-张家洼子区块

There is a close relationship between occurrence of nonmetallic minerals and tectonic evolution of geosyncline,platform and diwaon the western margin of the Dongting diwa .

洞庭地洼西缘非金属矿产的产出特征与地槽、地台及地洼构造的演化具有密切的关系。地洼构造对区内大部分非金属矿产的形成和保存是极为有利的。

Hybrid diwa-type orogeny which is the most common is composed of the former two types in space or in time.

在壳体构造理论下，笔者将地洼型造山运动定义为后地台阶段的构造—岩浆活化过程中各种地质作用的总称，并根据其动力来源和壳体运动方式，将地洼型造山运动划分为汇聚式、离散式和混合式，其中混合式是前两类型在时间或空间上的交替，最为常见。

The precambrian protodiwa was discoveried in China for the first time. In author's opinion, this region experienced a protodiwa staye with drastic Tectono-Magmatic Activiation Similar to the diwa region in phanerozoic thime. This achievement is an important contribution to the diwa theory.

在我国首次发现前寒武纪原地洼区，认为该区在晋宁运动后，经历了一个与显生宙地洼区相似的强烈构造—岩浆活化的原地洼阶段，对地洼学说作出了重要的贡献。

The high-resolution sequence stratigraphical framework of Sha-3 member in the central sag of Dongying Depression was established.

对东营凹陷中央洼陷带的钻井和三维地震资料进行了综合解释和分析，研究了东营凹陷中央洼陷带沙三段高分辨率层序地层格架。

Recently, the new found of archaeologic ingredients shows, the worship of jade tradition in ancient China is related to the archaeology culture of xiliaohe river area, the jade ornament of Hongshan culture, as well as xinglongwa culture, is the product of social religion life at that time, this paper will talk about the inner relationship between the jade ornaments of xinglongwa culture, hongshan cultrue in xiliaohe river area and China Etiquette Civilization.

近年来的考古新发现材料表明，中国古代源远流长的尚玉传统，追根溯源，与史前东北地区西辽河流域的考古学文化密切相关，红山文化的玉器，与兴隆洼文化玉器一样，都是当时社会政教礼仪生活的产物，史前西辽河地区兴隆洼文化和红山文化玉器群与中华礼制文明的内在关系问题值得关注。

According to core observation and description, many deformation structures with seismite characteristics are recognized within sandstone and shale sedimentary strata of Paleogene continental faulted basin in Yangxin Subsag, such as micro-faults, earthquake fissures, liquefaction sandstone veins, water-escape structure, vibrational liquefaction deformation structure, seismic pillow structure and associated structure, etc. The vertical sequence of seismites in Yangxin Subsag, in ascending order, is underlying unshocked layer, micro-faults layer, autoclastic shattered breccia layer, vibrational liquefaction deformation structure layer, seismic pillow structure and associated structure layer, liquefied homogeneous layer and overlying unshocked layer, which corresponds to different earthquake intensity respectively.

通过岩心观察和描述，在阳信洼陷古近系陆源碎屑断陷湖盆砂泥质沉积地层中识别出大量具有震积岩特征的变形构造，如微断层和震裂缝、水下岩脉和泄水构造、振动液化卷曲变形构造、震积枕状层及伴生构造等，同时建立了阳信洼陷震积岩垂向序列，自下而上分别是下伏未震层段、微断层层段、震碎角砾岩段、振动液化卷曲变形层段、震积砂枕及伴生构造层段、液化均一层段和上覆未震层段。

Lithologic character of Eogene syste is interbedded sandstone and mudstone primarily, including the thin layer oil shale, Neocene- Quaternary system is set of rivers deposits. Based on this, through the reaserch of ateral correlation and distribution characteristics of every structural layers show that: Paleozoic synthem overall thickness of relatively stable.The residual thickness of Mesozoic synthem is difference in the horizontal, Residues in the horizontal thickness of greater difference, to the greatest thickness achieve to 4500m. Eogene syste has obviously fault depression basin deposition characteristic, the thickness of many sags achieve to 3000 m ,from Neocene, the stratum crosswise mop tended to be stable.

在此基础上，通过对各构造层横向对比以及展布特征的研究表明，古生界构造层整体厚度相对稳定，冷武-奥陶系残留厚度在1200m左右，石炭-二叠系残留厚度在800m左右；中生界构造层残留厚度在横向上差异较大，最大厚度达到4500m，其中，下-中三叠统仅发育于南部小部分地区，最大厚度在1000m以上，侏罗系-下白垩统整体具有南厚北薄的展布特征，南部冠北洼陷厚度最大，达到3500m；新生界古近系具明显的断陷式盆地沉积特征，多个洼陷厚度在3000m以上，新近纪以后地层横向展布趋于稳定。

This one mode pays close attention to network credence foundation of the businessman very much.

这一模式非常关注商人的网络信用基础。

Cell morphology of bacterial ghost of Pasteurella multocida was observed by scanning electron microscopy and inactivation ratio was estimated by CFU analysi.

扫描电镜观察多杀性巴氏杆菌细菌幽灵和菌落形成单位评价遗传灭活率。