Based on detailed field observation and analysis on the large-sized Dongguashan copper deposit in the Tongling area, Anhui Province, it is suggested that the Dongguashan deposit is a large copper deposit formed by superimposition of the Yanshanian magmatic mineralization on the Hercynian synsedimentary massive sulfides.
作者中文名：曾普胜；裴荣富；侯增谦；蒙义峰；杨竹森；田世洪；徐文艺；王训诚摘要：通过对安徽铜陵地区冬瓜山大型铜矿床详细的野外观察和室内分析对比，笔者认为，冬瓜山矿床是一个海西期同生沉积的块状硫化物被燕山期岩浆成矿作用叠加而形成的大型铜矿床。
Faults formed in the Caledonian stage, the Late Hercynian Stage and the Himalayas Stage.
断裂的3次形成期为加里东期、华力西晚期和喜山期。
Based on the regional tectonic evolution, combined with the high precision isotopic ages from this paper and other geologists, we have some new acquaintances as follows: 1 There has no Caledonian granite belt distributed in north margin of North China Craton. So, the traditional evolving model of North China Carton, which formed on this idea and the acquaintance about the collision of North China plate and Siberian plate, must be incorrect; 2 The age date show that the earliest magmatic activity began since late-Palaeozoic Permian, which is inconsistent with the previous idea that there were Caledonian and Hercynian active continental margin in the north of North China Craton and in the south Xingkai Massif. 3 the crust and lithosphere were thickened by the subduction and collision of Siberia plate and North China plate during Late Paleozoic. The magma is formed when the crust is heated and melts caused by thickened lithosphere delamination and caused the Asthenosphere upwelling. But only a little basaltic magma erupted, most magma underplate under the bottom of the crust. Thermal energy derived from basaltic magma underplating made the middle and lower crust melt partially and the late Permian-early Triassic granites is formed in large scale.
根据区域构造演化分析，并结合本文及他人高精度同位素年龄，我们对延边花岗岩形成的大地构造环境有了新的认识：1在华北地台北缘并不存在所谓的加里东花岗岩带，因此，建立在此之上的传统的华北地台北缘演化模式及有关西伯利亚板块与华北板块的碰撞拼合的认识也必然是不正确的；2华北地台北缘和兴凯地块南缘不存在加里东期和海西期花岗岩带，表明两地块边缘最早的花岗质岩浆活动始于晚古生代的二叠纪，即不存在传统观点所认为的加里东期或海西期活动陆缘；3晚古生代由于西伯利亚板块与华北板块的俯冲碰撞，致使地壳和岩石圈增厚，导致加厚岩石圈发生拆沉作用，使得软流圈上涌，加热地壳使之熔融形成岩浆，但玄武质岩浆少量喷出地表，大部分底侵于地壳底部，形成下地壳高密度的玄武质底侵层，玄武质岩浆底侵的热能引起中下地壳广泛部分熔融，形成大面积分布的晚二叠世—早三叠世花岗岩。
Most of gold deposits were formed in collide-ductile shear processes, which was be tween Tarim plate and Junggar palte during Late Hercynian. The gold ore deposits were controlled by reginoal left-shear process.
金矿床形成于海西运动晚期发生的塔里木板块和准噶尔板块之间的碰撞—韧性剪切作用，而主要金矿床的就位受区域左行剪切作用动力学机制的控制。
The dating results of captured zircons show that the Middle-Late Jurassic (155-169 Ma), Indosinian (218-236 Ma), Hercynian (254 Ma, 294 Ma), Caledonian (413 Ma), and Precambrian (1823 Ma and 2542 Ma) magmatic events had taken place in the basin basement, which is consistent with the zircon U-Pb dating results from the basin basement rocks.
捕获锆石的定年结果显示，本区基底中存在中晚侏罗世(155~169 Ma)、印支期(218~236Ma)、海西期(254 Ma、294 Ma)、加里东期(413 Ma)和前寒武纪（1823 Ma 和2542 Ma）岩浆事件，这与基底岩石中锆石U-Pb的定年结果相吻合。
This study also suggests that the Wuchuan-Sihui fault zone may have been formed in the Hercynian-Indosinian Period, from which began its complex structural movement history.
同时也说明了吴川―四会断裂带可能是在海西―印支期形成并开始了其复杂的构造活动历史。
The formation age of Baishanzhi granodiorite measured by U-Pb method is 370±25 Ma, indicating the Hercynian period.
笔者首次利用锆石U-Pb方法测得白山子花岗闪长岩的形成年龄为370±25 Ma，属于华力西期。
Hercynian early, with the south of margin of Siberia plate submergence, Maici and Kelang volcanic Sedimentary basins were formed in the South of Altai mountain.
海西早期，西伯利亚板块南缘沉降，阿尔泰山南缘受到北西、南东方向张剪应力作用发生拉张，在D〓k〓阶段形成麦兹和克朗火山沉积盆地。
5Oil and gas were controlled by the structure formed by superposition of tectonic movement in the early and late Hercynian which resulted in palaeogeomorphology and degree of fracture growing. The latter decided the flowing direction of palaeocurrent and the degree of corrosion, which is the main factors of karstification. Especially, the superimposition of palaeostructure and Akekule uplift is the most favorable area for karst and fracture growing. The ubiquitous high angle fracture made all kinds of vugs into a large scale storage, so the fracture-vug system was divided into some blocks in the main oil zone on the plane.
5塔河油田的油气分布受控于海西早、晚期构造运动叠加形成的构造格架，古构造叠加的结果控制了古地貌和裂缝发育强度，古地貌和裂缝发育强度控制了古水系的流动方向及溶蚀深度，它们是岩溶作用发育的主控因素，特别是海西晚期形成的古构造与阿克库勒凸起轴部的叠合部位是岩溶、裂缝最发育的地区，普遍存在的高角度裂缝在三维空间将各类岩溶孔洞连通为大规模的储集体，从而造成主油区大型缝洞系统横向上的分区性。
Four phases of structural deformation are recognizable:the lst-phase structural detachment from SWW towards NEE occurred in Hercynian times; the 2nd-phase NE sinistral strikeslip movement took place in the Hercynian-Indosinian Period; while in the 3rd and 4th phases, ductile and brittle thrust faulting towards southeast happened respectively in area occupied by three secondary faults during Early Yanshanian and Himalayan times.
识别出四期构造变形：第一期为海西期的SWW→NEE构造滑脱作用；第二期为海西―印支期的NE向左行平移剪切作用；第三、四期分别为燕山早期和喜马拉雅期的NW→SE逆冲作用，且都发生在三条次级断裂地带。
Give full play to the mapping results in social development, the role of Hercynian building.
充分发挥测绘成果在社会发展、海西建设中的作用。
This is the depth study and practice the scientific concept of development and accelerating the construction Hercynian important results.
这是深入学习实践科学发展观、加快推进海西建设的重要成果。
I gave a construction for Hercynian poor power!
因为我能为海西建设献出一份微薄的力量！
Story 1: Northwest whirlwind couple of days ago was now Hercynian bright visit, it is.
故事一：前两天曾经的西北旋风，现在的海西亮来访，就是这样。
So the meeting in Xiamen, he personally, contribute to a better situation to determine the concept of Hercynian.
所以这次在厦门开会他亲自出马，有助于更好的判断海西概念的情况。
We believe that the two-center in Shanghai and have been granted after the Hercynian District, Shenzhen reform program is expected to be approved.
我们认为，在上海双中心和海西区相继获批之后，深圳改革方案也有望获得批准。
Zhejiang Hercynian Electronics Co., Ltd. was founded in 1998, specializes in the development of the game entertainment company.
浙江省海西电子有限公司创建于一九九八年，专业从事娱乐游戏机的研制工作公司。
5 Ma. These isotopic data provide important evidence for solving the problem of whether there occurred Caledonian mineralization and further support the view that pegmatites and pegmatite rare metal-muscovite deposits in the Altay area were not only formed in the Hercynian.
本次工作通过野外调查和同位素年代学研究，首次在阿尔泰西部的也拉曼大型含绿柱石白云母矿床(426±13Ma)、阿尔泰中部的那森恰大型含绿柱石白云母矿床(447.7±0.4Ma)及阿尔泰东部的青河拜兴白云母伟晶岩脉(436.0±0.5Ma)中获得了可靠的加里东期成矿的同位素年代证据，从而为解决是否存在加里东期成矿的问题提供了重要依据，并进一步认识到阿尔泰地区的伟晶岩及伟晶岩型稀有金属-白云母矿床并非只形成于海西期。
Researches on regional ore-forming process show that the major tungsten ore-forming event of the deposit occurred during the early Hercynian orogeny (322 Ma).
钨矿化的发生时间为海西期(322~260Ma)，其中云英岩型钨矿石的形成时代略早於黄玉－石英脉型矿石。
Each section has different structural characteristics. It`s north boundary is the Xialei-Lingma fault zone, the south is the Pingxiang-Dongmen fault zone.(5)The paleostress field characteristics in reserch behaved that, mainly near south to north compression folding-uplift movement in Caledonian orogeny, and also in Indosinian orogeny, west-north to east-south in Hercynian orogeny and in early Yanshan orogeny, north-eastnorth to south-westsouth in late Yanshan orogeny, east to west in early Himalayan orogeny and south to north in late Himalayan orogeny.
5研究区的古应力场特征表现为：加里东运动主要为近南北向的挤压褶皱-隆升作用；海西运动主要为北西-南东向的挤压褶皱作用；印支运动主要为近南北向的挤压褶皱作用；燕山早期运动主要为北西一南东向的挤压；燕山晚期运动主要为北北东-南南西方向的挤压；喜山早期运动主要为近东西向挤压；喜山晚期为近南北向挤压。