1) Arhada Ag-Pb-Zn camp
阿尔哈达银铅锌矿床
2) Arhada Pb-Zn deposit
阿尔哈达铅锌矿
1.
Arhada Pb-Zn deposit occurs mainly in cataclastic zone of Devonian System and ore bodies are dominated by blind ones in en echelon and locally cut with each other.
阿尔哈达铅锌矿主要产于泥盆系的NW向断裂破碎带中,矿体具雁行排列、局部交叉产出的特征,以盲矿体为主;成矿早期可能以岩浆热液(399~407℃)为主,而中、晚期的热液以大气降水或混合水(194~287℃)为主;硫分别来源于岩浆热液、沉积地层和大气降水;铅同位素测试结果则显示了成矿(岩)物质的混源特点。
2.
Arhada Pb-Zn deposit is located in strata of Devonian and Permian System near intermediate-acidic intrusive rocks and controlled by the NE fault-traversed sub-scale faults.
阿尔哈达铅锌矿产于中酸性岩体附近的泥盆系、二叠系中,受与NE向断裂贯通的成群(组)出现的次级断裂控制;矿体连续性较好,平面上呈透镜状,空间上呈柱状、似板状、透镜状,矿体为隐伏-半隐伏状,埋深不大;矿床属于中低温热液矿床。
3) Ag-Pb-Zn deposit
银铅锌矿床
1.
Geologic features,ore-hunting indicator of the Deerbuer Ag-Pb-Zn deposit;
得耳布尔银铅锌矿床地质特征及找矿标志
2.
Petrochemistry and Sr, Nd isotopes of intrusive in Lengshuikeng porphyry type Ag-Pb-Zn deposit;
冷水坑斑岩型银铅锌矿床含矿岩系岩石地球化学及Sr、Nd同位素研究
3.
Relationship between fluid inclusions and ore-forming of Jiawula Ag-Pb-Zn deposit in Hulunbeir league,Inner Mongolia
内蒙古呼盟地区甲乌拉银铅锌矿床流体包裹体与成矿的关系
4) Lead-zinc-silver deposit
铅-锌-银矿床
1.
The Bajiazi lead-zinc-silver deposit bears similar feature.
而八家子铅-锌-银矿床具有此类似特征。
5) Pb-Zn-Ag deposits
铅锌银矿床
1.
Many Pb-Zn-Ag deposits are found in the middle north margin of North China Block.
华北地块北缘中段分布着许多大中型铅锌银矿床,依据其成因特征可划分为四种类型:沉积喷气型矿床、叠加改造型矿床、与大红峪期碱性火山活动有关的浅成低温热液矿床、与中生代火山-斑岩活动有关的热液矿床。
2.
Four types of Pb-Zn-Ag deposits occur in the middle north margin of North China Block.
华北地块北缘中段是我国铅锌银矿床的重要富集区之一。
6) Pb-Zn-Ag Deposit
铅锌银矿床
1.
This paper presents an analysis of objective attributes in geology,geochemistry,and geophysics that occur in different sequences of the known mineral deposits,and of the metallogenic geological attributes in the Pb-Zn-Ag deposits in the northem Hebei Province.
通过对已知矿床不同级序的地质、地球化学和地球物理等客观属性的分析，研究了冀北地区铅锌银矿床成矿的地质要素。
2.
Yingfang Pb-Zn-Ag deposit lies in a S-N direction medium ductile shear zone,its mainore body occurs in the contact zone between coarse Or-granite of early Yanshanian andHongqiyingzi Group of Lower Proterozoic.
河北丰宁营房铅锌银矿床产于一近南北向的中型韧性剪切带中。
3.
Shidonggou Pb-Zn-Ag deposit exists within the external contact zone of Yeniutan granodiorite in-trusive,and is controlled by Shidonggou faulted structure.
石硐沟铅锌银矿床赋存于野牛滩花岗闪长岩侵入体外接触带中,矿床严格受石硐沟断裂带构造控制,矿化带长4 770m,矿体在矿化带中具分段赋存特征,而矿床中成矿元素具有从中温向中低温富集特征。
补充资料：哈达佛寺遗址
哈达佛寺遗址 ，Ruined Buddhist Temples at阿富汗古代佛寺遗址。在阿富汗东南部的贾拉拉巴德。年代为公元2～8世纪。中国古代僧人法显和玄奘曾访问这里。20世纪20年代发掘。经发掘的佛寺大多数只有塔院，院落为正方形，中心建主塔，四周是成列的小佛堂，院内有陆续建成的供养小塔。寺院内的塑像用黄白色石膏制成，有佛、菩萨、僧人、俗人、神怪等。塑像形象逼真，手法写实，技术熟练，具有明显的古希腊罗马风格，属犍陀罗佛教造像的西部地区派别。 |
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