古

The analysis from regional correlation indicates that the buried hill paleo-karst reservoir of also occurs in Bachu swell area, especially in area between Mazhatag fault and Tumuxiuke fault of the mid-upper seclion of Yingshan formation, compared with the paleo-karst reservoir developed in the upper section of Yijianfang formation of Middle-Lower Ordovician in throughout the whole Tarim basin in late of Middle Ordovician to early of Late Ordovician.

区域对比分析表明，推测巴楚凸起区特别是玛扎塔格断裂带与吐木休克断裂带之间的地区也广泛分布了该鹰山组中上部古潜山岩溶储集层，在塔北隆起区与之相当的是发育于中下奥陶统一间房组上部的古潜山岩溶储集层。

In the Paleozoic era,the northern border area of North China Craton belonged to the tectonic domain of south peri-Paleozoic ocean and is characterized by subduction-collision orogenesis,leading to the formation of EW- to ENE-trending folds,thrust faults,nappes and ductile shear zones etc.

古生代，华北地块北缘处于古亚洲洋构造域，造山作用属陆缘俯冲-碰撞型，形成以EW向至NEE向为主的褶皱、逆冲推覆构造及韧性剪切带等构造类型。

In the west, the study on people was started in ancient Greece in early times. But it studied people mainly on the basis of the relations between the man and nature, the man and deity.

在西方，关于人的研究早在古希腊就已开始了，但古希腊主要是在人与自然、人与神的关系层面上讨论人自身的问题。

Under the influence of the skeptics, Augustine eventually rejected Manichaeism as a religion and then discovered Plotinus, through whose writings he became a devout Neo-Platonist, arguing on behalf of Plotinus's semi religious interpretation of Plato.

在怀疑论学派的影响下，奥古斯丁最终放弃了摩尼教作为其宗教信仰，转而研究普诺提诺的作品，从而成为虔诚的新柏拉图主义者。奥古斯丁信奉普诺提诺关于柏拉图近于神圣的解读，并为之而极力奔走。

In the convergent processes of Pangia in Late Paleozoic, Tarim massif, Kazakhstan-Yili plate, Siberia plate, North China plate all amalgamated in Paleo-Asiatic tectonic domain.

在晚古生代Pangia的聚合过程中，塔里木地块和哈萨克斯坦-伊犁板块、西伯利亚板块、华北板块等在古亚洲构造域的造山过程中拼合在一起。

Part I described the Pelagian and semi - Pelagian heresies which Augustine sought to refute; Part II expounded Augustine's interpretation of man's original state of innocence and his subsequent fall; and Part III set forth his doctrine of salvation through God's redeeming grace in Jesus Christ.

第一部分介绍了pelagian及半-p elagian的歪理邪说，其中奥古斯丁试图反驳；第二部分阐述了奥古斯丁的解释人的原始状态无罪推定和他随后下降；和第三部分提出了他的学说的救赎通过上帝的救赎恩典在耶稣基督。

Translations of Augustine's works can be found in numerous sources, including Ancient Christian Writers; Catholic University of America Patristic Studies; The Works of Aurelius Augustinus; The Fathers of the Church; Library of Christian Classics; and A Select Library of Nicene and Post-Nicene Fathers.

翻译奥古斯丁的作品，可以发现在众多的来源，包括古代基督教作家；天主教大学，美国教父的研究；工程奥里利乌斯奥古斯丁；的父亲教会；图书馆基督教的经典；和一个专责图书馆尼西亚和后尼西亚父亲。

Translations of Augustine's works can be found in numerous sources, including Ancient Christian Writers; Catholic University of America Patristic Studies; The Works of Aurelius Augustinus; The Fathers of the Church; Library of Christian Classics; and A Select Library of Nicene and Post-Nicene Fathers.

翻译奥古斯丁的作品中可以找到许多来源，包括古代基督教作家；美国天主教大学研究教父；的作品奥里利厄斯奥古斯丁；的父亲教会；图书馆的基督教经典；和A选择图书馆尼西亚与后尼西亚父亲。

Of the five stages deformation, the exact ages of the (2) and (3) were determined by 40Ar/39Ar method as 290 and 259 Ma respectively.2. New results on the metamorphic belts and associated metamorphism of the Xiaopu metamorphic rocksBased on detailed microtextural observations and occurrence of typical metamorphic minerals, five metamorphic belts in the Xiaopu metamorphic rocks are identified. From the north to the south, they are biotite belt, garnet belt, staurolite belt, andalusite belt, and sillimanite belt. I suggested that the metamorphic belts occurred in the Xiaopu area belongs to the high temperature/low pressure series, may have resulted from the later Permian crust extension at ca. 290 Ma.3. I suggest that there may have been a Carboniferous backarc basin along the southern slope of the Harlik Mountain.Detrital Zircon SHRIMP U-Pb dating indicated that the sedimentary age of the Julideneng formation lithic sandstone must be later than late Devonian, most likely is Carboniferous rather than previously thought Precambrian. Analyses on its geologic setting, location of provenance, and sedimentary environment suggest the Carboniferous strata may form in a lagged backarc basin bounded by backarc uplifts.5. Reconstruction of the post-Paleozoic tectonic evolution history of the Harlik MountainThe tectonic evolution of Harlik mountains since the Paleozoic were reconstructed as followings:(1) arc-affinity magmative activities occurred during the middle-Ordovician to early-Silurian;(2) the middle-Silurian to late-Devonian was a back-arc uplift stage;(3) back-arc extension featured the Carboniferous period;(4) post-collisional extension and/then compression during Permian;(5) at the Mesozoic, differential uplift developed; and (6) the late Cenozoic is the intra-continental re-orogen stage.6. Primary estimation of the crust shortening is madeThe folded pre-Mesozoic strata were used to estimate crust shortening along the Harliknanshankou-Koumenzi, Shichengzi-Baishitou, and Qincheng-Xiaopu sections. Their shortening ratios are 16.2%, 19.8%, and 20.1% respectively corresponding crust shortening are 4.3, 9, and 11.3 km.

根据Ar-Ar热年代学研究，精确测定了早二叠世伸展变形和晚二叠世挤压变形的峰期时代分别为290Ma和259Ma.2、提出了关于哈尔里克山南麓小铺一带变质带和变质作用的新认识根据显微观察资料和特征变质矿物的出现，把小铺一带的变质岩由SW向NE方向依次划分为黑云母带、石榴石带、十字石带、红柱石带和矽线石带等变质带；初步确定该区的变质作用属于中温-低压型，变质作用发生的时代为290Ma左右，是该区早二叠世地壳伸展的产物。3、首次提出哈尔里克山南麓在石炭纪可能发育弧后盆地的新观点根据哈尔里克山南麓原&居里得能组&岩屑砂岩的碎屑锆石SHRIMP U-Pb定年，确认这套地层的沉积不早于晚泥盆世，很可能是石炭纪，而不是前人所说的前寒武纪；结合对其区域地质背景、源区位置和沉积环境分析，推测该区石炭纪可能为滞后弧后盆地和弧后隆起区构造背景。4、进一步证明哈尔里克山不发育与岛弧演化相关的泥盆纪岩浆活动根据对代表性闪长岩和花岗岩的锆石SHRIMP年代学研究获得的新资料，结合该区已有相关资料的综合研究，确定哈尔里克山岩浆岩分别形成于奥陶纪-志留纪和石炭纪晚期-二叠纪，不存在泥盆纪的岩浆岩，进而认为该区泥盆纪不属于岛弧环境。5、重建了哈尔里克山古生代以来的地质演化过程根据区域资料以及本次研究所获得的资料，把哈尔里克山古生代以来的构造演化划分中奥陶世-早志留世为岛弧、中志留世-晚泥盆世为弧后区、石炭纪弧后伸展、二叠纪为后碰撞伸展与挤压、中生代差异隆升和晚新生代陆内再造山过程等构造阶段。6、初步估算了哈尔里克山地壳缩短率和缩短量根据前中生代地层褶皱估算的哈尔里克山南山口-口门子、石城子-白石头和沁城-小铺三条剖面的地壳缩短率分别为16.2%、19.8%和20.1%，相应的地壳缩短量分别为4.3km、9km和11.3km。

An attempt has been made in present paper to advance the early periodic evolution of the earth crust in this region in four stages, by studing and analyzing the features of regional geophysical fields; the constitutional feature, division and correlation of early Pre-Cambrian strata of this region; the facies, formation and palaeogeographical environment; the development and evolution of palaeotectonic deformation and its control of the metamorphic iron ore.

本文从区域地球物理场特征、本区前寒武纪早期地层的组成特点和划分对比、岩相建造古地理环境、古构造变形及其对变质铁矿的控制作用，提出本区地壳早期演化分为四个阶段：1。

Do you know, i need you to come back

你知道吗，我需要你回来

Yang yinshu、Wang xiangsheng、Li decang,The first discovery of haemaphysalis conicinna.

1〕 杨银书，王祥生，李德昌。安徽省首次发现嗜群血蜱。