尖灭

Based on analyzing the test data ,three variety types of isothermal adsorption and desorption curves are confirmed . The first type is that the hole structure is provided with slit capillary bore the second is usually the type of upgrowthing one end nipped unparallel crevice the third belongs to the pores shaped " inkpot ".

在测试数据分析的基础上，确定了等温吸附和脱附曲线3种类型：第1类属孔结构是具有平行权构成的狭缝毛细孔型；第2类为发育一端尖灭的不平行的裂隙型；第3类属"墨水瓶"型孔。

This change may be showed on graph of level or altitude interval. The graph inflexion is the small structure's starting or ending.

这种变化可以从两条巷道中线水平间距或者曲线图反映出来，曲线图上的拐点即为小构造出现的位置或尖灭点。

The oil field lie on top wall override fringe of the Ke-Wu Rupture, belong to rupture screening type monocline pool, pool incline to east-west, angle of inclination is from 4°to 9°, the structure is simple.

该油藏位于克～乌断裂上盘超覆尖灭带上，属断裂遮挡的单斜油藏，油藏倾向于东西向，倾角4°～9°，构造单一。

In the study area, the thinning-out line of albic horizon is coincident with the 55.74m contour line, and the maximum horizon error was less than 1m and the maximum vertical error less than 0.04m.

基于湿地边界标准的湿地的定义应为：湿地是陆地和水体之间的过渡带，是由于地表淹水／土壤水饱和而形成的一种隐域性自然综合体，其上界位于陆地土壤诊断层的尖灭点处，其下界是有根植物下界。

The heavy oil in Wuxia area distributes in Mesozoic overlap pinchout on the upthrown fault far from Mahu oil sources, presenting arc distribution with conventional oil.

乌夏地区稠油分布于距油源玛湖凹陷远距离的断裂上盘中生界超覆尖灭带上，与正常原油呈弧状分布。

In later Guantao Formation, compression is primary, the maximal principle stresses no more than 0.1 MPa, and in central of Jiyang Depression horizontal shear stresses are dextral displacement, but sinistral displacement showed in west and east.

馆陶组油气藏都是它源性油气藏，断层是油气垂向运移的主要通道，盆地主要断裂系统控制油气垂向和平面上的分布，断层活动形成的披覆背斜，断鼻、断块构造，岩性尖灭是馆陶组主要的油气圈闭类型。

In this paper,a combined study was curried out for interpreting structure,distribution and tension of fault, wave field effect, heat state and nonelastic medium by explosion seismic Sounding, ZD and 3D long period surface waves of earthquake,magnetotelluric deep sounding,heat flow survey,the mechanism of tectonic movement and deep internal processes in Qinghai-Xizang Plateau.

地壳到地幔速度结构的纵向结构变化，横向分区和走时残差随深度的显著变化，板块边界的地球物理异常场效应，垂直向差异显著的地壳结构与深大断裂体系，低速层的变异、分布、尖灭与缺失，以及近代火山活动地区典型的地热活动特征等，不仅说明构造异常，而且也说明了青藏高原地壳与上地幔在纵向与横向上都不均匀。

The predicted sand bodies are distributed in north-cast and approximately north-south orientation. The sandstone reservoir, which is getting thin and pinch out to the high west-north structure, is easy to form the lithological trap with sand body updip pitchout and the structural lithologic trap. Lens sandstones developed and are distributed in source rocks, It is easy to form lithologic traps.

预测砂体分布呈现出北东向、近南北向展布特征；向西北构造高部位方向变薄尖灭的储集砂体极易形成上倾尖灭岩性圈闭及构造－岩性圈闭，透镜体砂岩也较发育，其分布于生油岩区，容易形成岩性圈闭。

Based on oil-gas distribution law, by means of correlation oil and sourcerock oil gonane isomeric parameter and relative content of pristane and tane, it draws to a conclusion that in west slope region oil of S oil layer mainly comes from K1qn sourcerock in Qijia-Gulong sag.

构造和构造-岩性油气藏主要分布在泰康隆起带的中南部；岩性上倾尖灭油气藏主要分布在富拉尔基地区。

Type of oil-gas reservoirs were dissected, the result shows that S_(2+3) oil layer inwest slope region have four types oil-gas reservoirs, anticline, lithotogic updip pithing, structural-lithologic,fault barrier. Gas lies upper but oil lies bottom in the same layer, oil-gas distribute mainly in Taikang upliftzone and nearby in the plane, the types of oil-gas reservoirs are anticline and structural-lithologic inTaikang uplift zone.

通过典型油气藏解剖得到西斜坡区萨二、三油层油气藏主要有背斜、岩性上倾尖灭、构造—岩性、断层遮挡4种类型油气减，同一油层气在上油在下，油气在平面上主要分布在泰康隆起带及其附近，泰康隆起带以背斜和构造—岩性油气藏为主，西部超覆带以不整合和岩性上倾尖灭油气藏为主。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。