穹隆

These blind regmagenesis were most level ones and showed some law to certain extend. They are the antimere to those that have been explored.

在小河～石门坎区段之间，存在一系列受火箭山穹隆控制的近东西向的放射状隐伏断裂，将隐伏矿切割、平移和错断，从而改变其连续性。

According to model, lead zinc ore bodies of mineral deposit, celestite ore bodies and gypsum ore bodies are distributed by the incomplete dome shape. The sandstone type ore bodies like a curved surface shape, is on the top, wide distribution, which like the top cover of a mushroom. The limestone breccia type ore bodies, under the sandstone type ore bodies, with mostly irregular vein shape, lens body shape, locate at the root of the mushroom. Gypsum and celestite ore bodies, accompanying with limestone breccia type ore bodies with the shape of vein, lens body, distribute under the sandstone type ore bodies.

根据模型显示，金顶矿床铅锌矿体、天青石矿体和石膏矿体呈不完整的穹隆状分布，砂岩型矿体在上，为曲面状，分布广，似一蘑菇的顶盖，而灰岩角砾岩型矿体分布局限，部分产于砂岩型矿体之下，多为不规则的脉状、透镜体状，构成蘑菇的根部；石膏和天青石矿体主要与灰岩角砾型矿体相伴产出，呈脉状、透镜体状，多分布于砂岩型矿体下部。

New data of structural styles and geochronometry in the Dulong-Song Chay metamorphic dome indicate at least two epoches of major extensional tectonics: the D, deformation of the rising and exhumation of the dome occurred at 237-228 Ma; and the D2 deformation overprinted and re-deformed on the dome at 86-78 Ma. Of them, the D, deformation shows a consistent forming time, extensional direction and tectonic regime amongst the Dulong-Song Chay dome, South China block and the north margin of the South China Sea basin.

对位于华南地块西南缘的都龙－Song Chay变质穹隆体的研究表明，在中生代至新生代时期，至少经历了2期重要的伸展构造：D1期(237~228 Ma)穹隆的隆升与表露阶段，代表了印支期造山作用前的伸展构造；D2期(86~78 Ma)叠加和改造阶段，并有可能始于176~146 Ma，致使穹隆进一步隆升和表露。D2期构造在发育时间、伸展方向及变形方式等上既与华南地块同时期区域伸展构造特征相一致，也与南海盆地北缘早期扩张特征相一致。

They were east-west direction and were incised, removed and cut and lose their continuum.

转向位置在水平面上，正东向对应于火箭山穹隆核心部位。

Salt Dome is a mushroom-shaped or plug-shaped diapir made of salt , commonly having an overlying cap rock .

盐丘是褶曲的平面形态中浑圆形褶曲的一种，穹隆构造，其核部为很厚的岩盐层，并刺穿上覆岩层，此种穹隆称为盐丘

The authors used gravity gradient anomalies to interpret the Southwest sea basin of the South China Sea and obtained the domal structure plane with the NE-trending spreading axis of the sea basin as the symmetric axis.

本文利用重力梯度异常对南海西南海盆进行了解释，得到大致以西南海盆北东向扩张轴为对称轴的穹隆状构造面。

Methods Health female Wister rats were randomly divided into the model group and control group with five rats in each group.The fimbria/fornix transection and ovaries cutting were simultaneously performed for the animal model.

将大鼠分为穹隆-海马伞切断组、去势组和假手术组，假手术组除了不切断穹隆-海马伞和去除卵巢外，其余步骤同模型组。

Methods Totally 20 health female rats were randomly and equally divided into control group, fimbria/fornix transection and ovariectomized group, ovariectomized group and fimbria/fornix transaction group.

取健康雌性Wistar大鼠20只，随机分成四组，对照组，穹隆海马伞切断加卵巢切除组，卵巢切除组，穹隆海马伞切断组每组各5只。

According to the tectonic setting and minefield structural features analyses,considered that the genetic mechanism of Hanxiecun small dome structure in Yaoshan minefield is a diapiric thermal dome.

根据区域构造背景及井田构造特征分析，认为尧山井田韩解村小穹隆构造的成因机制为底辟式热穹隆构造。

Built geodesic dome , geodesic dome , dense grid, dome , geodesic dome , polyhedral dome .

测地线拱顶，短程线拱顶，密网格穹隆，网格球顶，多面体穹窿。

The absorption and distribution of chromium were studied in ryeusing nutrient culture technique and pot experiment.

采用不同浓度K2CrO4(0，0.4，0.8和1.2 mmol/L)的Hoagland营养液处理黑麦幼苗，测定铬在黑麦体内的亚细胞分布、铬化学形态及不同部位的积累。

By analyzing theory foundation of mathematical morphology in the digital image processing, researching morphology arithmetic of the binary Image, discussing two basic forms for the least structure element: dilation and erosion.

通过分析数学形态学在图像中的理论基础，研究二值图像的形态分析算法，探讨最小结构元素的两种基本形态：膨胀和腐蚀；分析了数学形态学复杂算法的基本原理，把数学形态学的部分并行处理理念引入到家实际应用中。