原生体

基本解释 (translations)

bioblast  ·  bioplast

与原生体相关的网络例句 [注：此内容来源于网络，仅供参考]

In animal and protoctist cells the centrosome contains two short barrel-shaped structures, the CENTRIOLES, but these are not directly involved in spindle formation.

在动物和原生生物的细胞中，中心体包含两个短的圆筒状的小体－中心粒，但它们和纺锤体的形成并没有直接的关系。

Study using infrared microtechnique reveals three types of fluid inclusions in rutile:Ⅰ-type aqueous inclusions,Ⅱ-type CO_2-H_2O inclusions and Ⅲ-type CH_4 inclusions. Primary and pseudosecondary type Ⅰ inclusions, as well as Ⅱ-type fluid inclusions, having a range of pressure between 0.6 and 1.3 GPa, were trapped during the amphibolite-facies retrogression stageof eclogites, suggesting that fluids related to rutile mineralization originated from water released during retrograded metamorphism of eclogites.

利用红外显微镜对金红石进行的流体包裹体研究表明，金红石中主要存在三类流体包裹体，即Ⅰ型H2O溶液包裹体、Ⅱ型CO2-H2O包裹体和Ⅲ型CH4包裹体，其中I型原生和假次生流体包裹体和Ⅱ型流体包裹体反映出的压力范围为0.6～1.3 GPa，与榴辉岩角闪岩相退变质作用的压力相当，说明与这类金红石形成有关的变质流体源于榴辉岩退变质作用所释放的水。

The mantle-derived peridotite inclusions with protogranular texture and porphyroclastic textures;(2) the pyroxenite inclusions with cumulate texture; and (3) the granulite and gneisses with crystalloblastic textures.

辽西的深源岩石包体也有三种结构类型：①具有原生粒状结构、残碎斑结构的幔源橄榄岩类岩石包体；②具有堆晶结构的辉石岩类包体；③具有变晶结构的麻粒岩和片麻岩类岩石包体。

During the magmas ascendedand intruded, the high-energy, quick ascending primary mantle magmas with xenolith andhigh-pressure megacrysts didn't react with the crustal matter, which formed products, such ascone sheets.

在岩浆上升侵位的过程中，能量高的快速上升的含有岩石包体和高压巨晶的幔源原生岩浆没有与地壳物质发生作用，其形成的产物如锥状岩席；在此之后，岩浆能量、上升速度的降低促使原生岩浆与围岩发生轻微的同化混染作用，其产物如火山熔岩和火山颈。

The bacterial bioplastic coating argument is the strongest, as there have been cases in which ancient textiles have yielded radiocarbon dates much younger than other artifacts in the same sites—most notably in the instance of mummy 1770 in the British Museum, whose bones dated 800 to 1,000 years older, according to the radiocarbon tests, than the textile in which they were wrapped.

细菌性的&原生体覆盖物&的争论来得更激烈，已经有案例，就是古代纺织品的放射性碳年代测定比其他同样大小的史前器物的年代要晚得多——最值得注意的例子就是1770年陈列在大英博物馆的木乃伊，根据放射性碳年代测定，骨骼的年代为800至1000年之久，它们都被包裹着。

Gove, the nuclear physicist at the University of Rochester who designed the carbon-dating technique used on the shroud, stated, There is a bioplastic coating on some threads, maybe most.

罗切斯德大学原子物理学家哈里在设计裹尸布测定技术的时候说过：&有一些原生体覆盖在细丝上，也许更多。&

Associated minerals are primary glauberite, halite and terrigenous mud; while calcite is absent or rare. The X-ray diffraction analysis shows that the mud-sized crystalline dolostone has an average CaCO3 mole content of 57.30% and an average degree of order of 0.40, revealing the characteristics of higher calcium content and lower degree of order. It is closely intergrown with glauberite, indicating that the aqueous medium in the depositional environment of mud-sized crystallinedolostone was hypersaline water or dilute brine. The temperature of water in the depositional environment calculated according to the oxygen isotope data averaged 30.5℃ and the minimum homogenization temperature of inclusions in primary glauberite crystals associated with mud-sized crystalline dolomite was 44℃. The two groups of temperature data are close, indicating that the temperature of the water in the paleolake environment during the deposition of mud-sized crystalline dolostone ranged from 30.5℃ to 44℃.

泥晶白云石在阴极发光下呈红色、橙红色，与其伴生的矿物除原生钙芒硝、石盐、陆源泥质外，方解石没有或极少；X衍射分析结果表明，泥晶白云石的CaCO3摩尔含量平均为57.30%，有序度平均为0.40，具高富钙、低有序的特征；与钙芒硝岩的紧密共生，说明泥晶白云岩沉积环境的水介质为高盐度的咸水或淡卤水；根据氧同位素数据计算的沉积环境的水体温度平均为30.5℃，与泥晶白云石伴生的原生钙芒硝晶体中的包裹体均－温度最低值为44℃，这两组温度数据基本接近，表明泥晶白云石沉淀时环境水体的温度大致在30.5-44℃之间。

By studying reservoir rock characteristics, diagenesis and physical property, investigation showed that there were distributary channel, branch channel, mouth bar, distal bar, sand sheet, lakeshore, shallow lake and limestone flat . we concluded that the reservoir of N1～N21 is low porosity and permeability reservoir with the types of primary porosity and secondary intergranular porosity, which is in the early diagenetic stage B into the late diagenetic stage A subperiod. The role of effecting reservoir physical property is deposition, cementation, dissolution and tectonic rupture. After researching of reservoir, we divided it into three categories and division the favorable facies belt and relatively favorable. We think that the favorable facies belt is braided river delta front and partly shallow lake in east of the Fault Ⅶ. favorable reservoir is in the first and the second class.

进一步研究了本区碎屑岩储层的岩石学特征、成岩作用特征、物性特征，研究认为该区储集体类型有分流河道砂体、分支河道砂体、河口坝、远砂坝、席状砂砂体、滨湖砂滩、浅湖砂坝砂体及灰坪；N1层属于低孔、特低渗储层，孔隙类型以原生、次生粒间溶孔为主；分析了影响储层物性的因素主要为沉积作用、胶结作用、溶蚀作用和构造破裂作用；进行了储层评价与有利相带预测，将储层分为三类并划分了有利区带、较有利区带，认为Ⅶ号断层以东的辫状河三角洲前缘亚相和部分浅湖亚相是N1的有利储集相带，储层以Ⅰ、Ⅱ类为主。

Reefs, reef-mounds and lime mud mounds are all carbonate buildups, and the reefs and banks are important targets for petroleum exploration The reefs, banks and mounds should be divided from each other not only in theory, but also in exploration practice, because of so many differences in sedimentary compositions, fabrics, environments, distribution in time and space, and the characteristics of petroleum geology If the original reef or bank itself was fine reservoir rocks, then it would become a better reservoir after the reservoirconstructive diagenesis The formation of a high quality carbonate reservoir is controlled by two factors: the sedimentary microfacies and the reservoirconstructive diagenesis The first is the basis for the formation of a high quality reservoir, and with the high energy reefbank facies as the best; the latter includes the cataclasis, the dolomitization and the karstification The dolomitization and karstification are the best for the formation of a high quality reservoir The karstification has the widest distribution, profoundest effect, and plays a vital role in the high quality reservoir forming The karst types are quite rich in the limestone reef or bank reservoir, including synsedimentary karst, penesedimentary karst, supergene karst and hydrothermal karst, and so does the dolomitization reef or bank reservoir The formation mechanism of synsedimentary karst and penesedimentary karst is related to the short time exposing and leaching of the cyclical highfrequency shallowupward sequence when the reefs or banks are forming The supergene karst is controlled by the exposing and leaching of tertiary cyclic sequence type I interface after the reefs or banks forming Thus, there developed a great deal of secondary corrosion pores, corrosion fractures and huge caves besides some original pores remained in the reef and bank reservoir Scarcely there are any original effective pores in reefmounds and lime mud mounds, especially in senkes among mounds, but secondary pores could be formed by karstification, and there would likely develop source rocks with high organic abundance

礁、礁丘、丘同属碳酸盐建隆，礁、滩是重要勘探目的层。但各自在沉积组分、组构、环境和时空分布，以及油气地质条件上迥然不同，因而无论从理论还是勘探实践上，都有必要将其各成体系划分开来。礁滩自身为好储集岩，当建设性成岩作用叠加后可形成好的储层。碳酸盐岩优质储层形成，主要受沉积微相与建设性成岩作用两大因素控制。前者是基础，并以高能的礁滩相带为最好；后者主要包括破裂、白云石化和溶蚀三大类，并以白云石化或溶蚀为最优，其中的溶蚀分布最广泛、影响最深刻而对优质储层形成起决定性作用。礁滩储层中的古岩溶类型最为丰富多彩，包括同生期、准同生期、表生期和埋藏期热流体岩溶的所有类型，白云岩化礁滩体也不例外。其中，同生准同生期岩溶的形成机制与礁滩沉积时高频层序旋回向上变浅序列的短暂暴露淋溶有关，表生期岩溶则受控于礁滩沉积后三级层序旋回Ⅰ型界面的暴露淋溶。由此，导致礁滩储层中除了可以也是唯一保存原生孔隙外，还发育了次生溶蚀孔洞缝和大型溶洞。礁丘、灰泥丘尤其是丘间洼地中发育高有机质丰度烃源岩；它们自身没有有效的原生孔隙，但岩溶作用可以形成次生孔隙。

By mitochondrial DNA control region sequencing the relationship of haplotype phylogenies can be reconstructed to distinguish the Taiwan ring-necked pheasant and imported ring-necked pheasant. Additionally, the sequencing can be used to analyze genetic diversity and genetic structure. The results are expected to provide the reference base for identifying and conserving Taiwan ring-necked pheasant.

本论文研究结论建议，未来进行原生环颈雉族群保育或人工复育计画时，可利用外部形质测量分析、粒线体DNA基因型与遗传多样性分析，做为环颈雉各原生或外来族群的个体辨识工具，并提供拟订族群保育及复育经营措施之参考依据。

与原生体相关的网络解释 [注：此内容来源于网络，仅供参考]

bioblast：原生体

biobenetic isolation 生物发生分离 | bioblast 原生体 | biocalorimetric 测定生物热量的

elementary body：原(生小)体

衣原体的生长发育周期分两个阶段:原生小体(elementary body),是发育周期的感染阶段;网状小体(initial body),是在感染细胞内的繁殖阶段. 原生小体先附着于易感细胞的表面,然后通过细胞的吞噬作用进入细胞内,形成网状小体在细胞内繁殖,

frond：藻体

紫杉叶蕨藻属绿藻植物门松藻目蕨藻科海草,型态包括假根(Rhizoid)、匍匐茎(Stolon)与藻体(Frond)等三大部分,因藻体酷似紫杉叶片而得名. 该种蕨藻原生於巴西、印尼、菲律宾、越南、坦桑尼亚等地之热带海域,原生型(native strain)之体型较小,

native：原生

否则须 等到并且买了 原生(Native)软体后才能用,特别须注意的是,您的周边设备驱动程式是否已相容?可以解释" 原生(Native)软体"是什麼意思吗?可以解释" 原生(Native)软体"是什麼意思吗?可以解释" 原生(Native)软体"是什麼意思吗?

protoplast regeneration：原生質體再生 原生质体再生

protoplast fusion 原生質體融合 原生质体融合 | protoplast regeneration 原生質體再生 原生质体再生 | protostane 原類固醇烷 原萜烷

primary sorbite：原生索氏体、一次索氏体

prestressed forming预应力成型法 | primary sorbite原生索氏体、一次索氏体 | prime cost成本

primary succession：原生演替

(1)原生演替(primary succession)开始于原生裸地或原生芜原(完全没有植被并且也没有任何植物繁殖体存在的裸露地段)上的群落演替. (2)次生演替(secondary succession)开始于次生裸地或次生芜原(不存在植被,但在土壤或基质中保留有植物繁殖体的裸地)上的群落演替.

protogenetic inclusion：原生包裹体,原生内含物

protocol 议定书,协议,(条约)草案 | protogenetic inclusion 原生包裹体,原生内含物 | protogenetic 原生的

Strongyloplasmata：原生小体

"软疣小体","Strongyloplasma homminis ; Molluscous bodies ; Molluscous corpuscles" | "原生小体","Strongyloplasmata" | "轻传染","Subinfection"

agglomerates：团聚体

球形或微晶组成的大晶体形式存在;凝聚体(aggregates)是由原生颗粒表面彼此吸附而成;团聚体(Agglomerates)是由原生颗粒或凝聚体疏松的组合,...