二叠纪的

Regarding the sytem territory of super sequence as a unit, and depending on more than two handred data points, the space-time distribution of lithofacies and paleogeography in six key periods of Permian and the filling characters of prototype basins are reveal.

以超层序的体系域为单元，依据200多个资料点，再造了二叠纪六个关键时期构造—岩相古地理的时空展布与原型盆地的沉积充填特征。

In the latter part of the Permian, smaller varieties emerged, likely warm-blooded and covered in insulating hair.

在二叠纪后期，个头小热血的有皮毛的爬行类出现了，这其中就有以后的哺乳类。

The Centr al Tethys Region lies in Hoh Xil-Bayan Har. Since Late Palaeozoic, the back-ar c bathyal basin continued to break and spread. The typical oceanic crust was event ually formed in Carboniferous and Permian. The Ocean during that period is named the Paleo-Tethys, of which the remnant is the Third and the Fourth suture zone s.

特提斯中区位于可可西里—巴颜喀喇，古生代晚期以来在弧后盆地基础上继续破裂、扩张，典型的洋壳形成于石炭—二叠纪，这个时期的洋称古特提斯，它的遗迹为第三和第四缝合带。

The representative fanna is that from Qingyan, Guizhou province, southwestern China, dated as Late Anisian, composed of nearly 100 species assigned to more than 50 genera, belonging to 32 families of 5 subclasses in Bivalvia.

研究了二叠纪未生物大灭绝事件后双壳类的首次辐射，辐射的代表是贵州青岩地区中三叠世Anisian晚期的青岩生物群，共50余属100余种，归在5亚纲10目18超科32科。

The chief controlling factors to available reservoir are paleo-karst morphology in Llandeilo to Early Caradoc and multi-stage faulting and karstificatio. Its evolution of reservoir chiefly suffered the reconstruction of diagenesis such as epidiagenetic karstifiration uncovered for over 10 Ma in Llandeilo to Early Caradoc and 3-stage burial karstification since Late Ordovician to Devonian, Permian to Triassic and Tertiary.

有效储集层主控因素是兰代洛世－卡拉道克世早期的岩溶古地貌及多期断裂岩溶作用，其储集空间演化主要经历了兰代洛世－卡拉道克世早期长达10×10^6a以上的暴露淡水岩溶及3期（晚奥陶世－泥盆纪、二叠纪－三叠纪、古近－新近纪以来）埋藏岩溶等建设性成岩作用的改造。

Pulling setting presents in southern China in Permian forming rift basins, which extends and develops from the edge to the inside of continent. Under the influence of Dongwu movement, two second order cycles forming by up and down of sea level happened in Yangtze and Huaxia craton. Rift basins in continental margin are primary sedimentary location of LST. But craton areas are the main deposition area of TST and HST. Weathering on land and river sediment or only thin coaly clasolite of marsh facies present mainly in LST deposition.

二叠纪我国南方总体处于拉张背景，发育了由陆缘向陆内延伸发展的裂陷盆地；受东吴运动影响，扬子和华夏克拉通遭形成了两个二级海平面升降沉积旋回；陆缘裂陷盆地是低位期沉积的主要场所，而克拉通区主要为海侵和高位期沉积，低位期主要表现为陆上风化残积、河流沉积或仅发育厚度很薄的沼泽相含煤碎屑岩。

Mao Jingwen%Wang Zhiliang%Li Houmin%Wang Chengyu, Chen Yuchuan Carbon and oxygen isotope components in the Permian basalt-hosted copper deposit in Ludian area, Yunnan:Implication for the mineralization process Geological Review , 2003,6

毛景文%王志良%李厚民%王成玉%陈毓川云南鲁甸地区二叠纪玄武岩中铜矿床的碳氧同位素对成矿过程的指示地质论评， 2003，6

Various log and core data are used to estimate the petrophysical parameters such as porosity and permeability, and to define the distribution and petrophysical properties of the framework sandbodies in each formations of the PermoCarboniferous in the Bohai Bay basin.

应用录井、测井及岩心资料，测定了孔隙度、渗透率等物性参数，查明了渤海湾盆地石炭-二叠系各地层组的骨架砂岩展布特征及其物性特征；应用相比法编图对渤海湾盆地石炭纪、二叠纪岩相古地理进行了恢复，研究了沉积相对储层及其物性特征的控制作用。

Late Permian to Triassic rifting and subsidence resulted in the deposition of as much as 9 kilometers of Triassic strata, locally injected with sills.

二叠纪晚期到三叠纪断裂和下沉作用形成了大约9千米厚的第三纪沉积地层，在其中有岩床的切入。

Restoration of paleo-geothermal field based on vitrinite reflectance in strata indicates that the paleo-geothermal of Pre-Permian strata in mineralization district of the Youjiang basin was up to above 280℃, and that of Triassic falls between 150℃ and 250℃.

通过地层中镜质体反射率值对古地热场进行恢复，确定右江盆地成矿区内二叠纪以下地层曾经所达到的古地温在280℃以上。而三叠纪含矿层段所达到的古地温在150℃-250℃之间。

On the other hand, the more important thing is because the urban housing is a kind of heterogeneity products.

另一方面，更重要的是由于城市住房是一种异质性产品。

Climate histogram is the fall that collects place measure calm value, cent serves as cross axle for a few equal interval, the area that the frequency that the value appears according to place is accumulated and becomes will be determined inside each interval, discharge the graph that rise with post, also be called histogram.

气候直方图是将所收集的降水量测定值，分为几个相等的区间作为横轴，并将各区间内所测定值依所出现的次数累积而成的面积，用柱子排起来的图形，也叫做柱状图。