schizocoel

The analysis of faults system and faults movement is the basement to research its sediment and structure evolve,types of trap and the characteristic of oil-gas migration and pool formation.

沾化凹陷四扣洼陷区是受张性及张扭性应力控制的箕状断陷区,断裂体系及活动特征分析是对其沉积构造演化、圈闭类型及油气运聚规律研究的基础。

The slope zone of Biyang depression developed many faults and has complicated faults system.

通过对斜坡带断裂体系特征及其控油规律研究 ,指出主控断层的发育规模、连续性及与砂体、鼻状构造走向的交切关系控制油气的运移、聚集模式和油气藏类型及丰度。

Multi-f ractal spectrum behaviour of fault system and its application;

断裂体系多重分形谱特征及其应用

Fractal characteristics and reservoir distribution of fault system in the northwest margin of Jungar basin;

准噶尔盆地西北缘断裂体系分形特征与油气藏分布

It is vertically divided into the deep fault system and the shallow fault system bounded by the bottom of Jurassic.

在垂向上,以侏罗系底界为界,将断裂划分为深层断裂体系和浅层断裂体系,由于深、浅层断裂体系活动时间和活动强度的差异,对油气成藏的控制作用也有明显的不同。

The complicated fracture systems and tectonic framework were formed in the central and southern parts of the South China Sea due to the reciprocal movement of the plates like the Euro-Asia Plate, the Pacific-Philippine Plate and the India-Australia Plate during Mesozoic and Cenozoic.

中新生代时期,欧亚板块、太平洋-菲律宾海板块、印度-澳大利亚板块等几大板块之间的相对运动和相互作用,导致南海中、南部形成复杂的断裂体系和构造格局。

Objective To observe the morphological characteristics of Plasmodium yoelii schizogony in their ghost erythrocytes.

结果鬼形红细胞内的疟原虫形态结构完整熏呈现红内期各期疟原虫的特征性结构,如红细胞膜源性纳虫空泡,指环样早期滋养体熏“褡裢”(brassiere)样早期裂殖体,裂殖体表面新生芽体和葡萄串样晚期裂殖体的外形;早期滋养体的胞口、食物泡和结晶样的疟色素颗粒,晚期滋养体的核质与核膜的增生熏及其增生核膜的衍化;裂体增殖过程中先行的团块样核分裂及其随后的芽体等头端结构的形成。

In the paper, some morphological and biological materials of a kind of Schistosoma obtained from mice or rabbits experimentally infected with cercariae from natural snail living in Nanjing are presented as follows: (1) Adult worms superficially resemble to Schistosoma japonicum but smaller in size.

用自然环境中钉螺逸出的尾蚴感染小鼠和兔 ,获得了一种比日本血吸虫小的裂体吸虫。

Research achievements in geology and geophysical deep survey have revealed that there are two fault systems of different generations in the Eastern Xinjiang and the Western Gansu.

地质、地球物理测深研究成果揭示新疆东部、甘肃西部存在两个世代、两种不同的断裂体制:深部断裂体制,形成于古生代,主要反映板块碰撞-对接前板块之间或板内不同块段之间的离散与聚合,控制古生代的构造格局;浅部断裂体制,形成于华力西晚期至中新生代,主要反映板块碰撞-对接后壳内强烈水平挤压,控制中新生代构造格局或逆冲-推覆-滑脱构造。