亚欧带东段和西段继续发生强震。
Strong earthquakes successively occurred on the eastern and western parts of the Eurasian belt.
竹林坡金矿位于秦岭造山带西段。
The Bamboo slope of Qinling orogenic gold deposit is located in the western section.
西段呈强显露型逆冲至地表。
The west fragment of structure thrusts up to ground surface.
地址：河北省秦皇岛市海港区河北大街西段。
Address: West part of Hebei Street, Haigang District, Qinhuangdao, Hebei.
靠近街道一侧，它与房子的西段伸出部分对齐。
On the street side, it's aligned on the advanced parts of the houses on the west.
羊露河上游铁矿位于北祁连西段加里东褶皱带西段。
Iron ore deposits in upper reach of Yangluhe river are situated in the west Calidonian fold belt of the west Qilianshan mountain.
铁岭—靖宇成矿带西段构造岩浆活动具有多旋回特点。
The tectonic-magmatic activity of the west of Tieling-Co-Jingyu mineralization belt had the features of multicycle.
四川黑水徐古锰矿位于日嘎希—瓦钵梁子复背斜西段北翼。
The Xugu Mn deposit in Heishui, Sichuan lies in the northern limb of the Rigaxi-Waboliangzi anticlinorium.
西段和中段表现为左旋走滑，东段表现为左旋走滑逆冲运动。
It shows sinistral strike-slip movement in western and middle segment, sinistral strike-slip and thrust in eastern segment.
寒山金矿位于甘肃北祁连造山带西段、阿尔金大断裂带南侧。
Hanshan gold deposit is located in the west part of north Qilian orogenic zone of Gansu, and south side of the Altyn fault belt.
黑刺沟金矿位于秦祁昆地槽褶皱系南祁连地向斜构造带的西段。
Heicigou gold deposit is regionally located at the western section of the southern Qilian geosyncline of QinlingQilianKunlunshan mountain fold system.
江西萍乡地区位于扬子地块和华夏地块两大构造单元对接带的西段。
Pingxiang area Jiangxi Province is in the western part of the junction between Yangzi and Huaxia Block.
进一步研究表明，西昆仑山地区西段中晚更新世至少经历了3次强烈的隆升。
Further study suggests that the western of the west Kunlun Mountains in the Mid-late Pleistocene has undergone at least 3 times strong upheaval.
由炉霍、道孚、乾宁三条次级断裂左阶斜列组合而成的鲜水河断裂带的北西段。
The northwest part of Xianshuihe fault consists of three subfractures which are Luhuo, Daofu and Qiannin Faults.
准噶尔盆地南缘中西段构造具有分带性，由山前到盆地可大致分为三排构造带。
The middle segment of the southern Junggar basin has three anticline belts from foreland to the basin with different type of structures.
寒山大型金矿是近年来在北祁连山西段发现的与侵入岩有关的构造蚀变岩型金矿。
The Hanshan gold deposit is a tectonic altered rock type deposit discovered recently in North Qilian Mountains.
喀拉玉尔滚右旋走滑断层为薄皮构造，调节了却勒地区东、西段前缘的变形差异。
Karayulgun dextral strike-slip fault, which is a thin-skinned structure, adjusted the deformation difference located at frontal range of Quele area.
寒山大型金矿是近年来在北祁连山西段发现的与基性火山岩有关的构造蚀变岩型金矿。
Recent discovered Hanshan gold deposit is a structure-controlled altered rock type related with intrusive rocks in North Qilian Mountain.
汝州煤田位于华北板块南缘逆冲推覆构造带豫西段前锋部位，区内逆冲推覆构造较发育。
The Ruzhou coalfield lies at the front part of thrusting nappe structural zone western Henan sector, south margin of the North China plate.
延吉石人金异常位于五凤—汪清—六道崴子金、铜成矿带西段，成矿地质条件十分有利。
The Shiren Au anomaly, Yanji is located in the western part of Wufeng-Liudaowaizi Au, Cu metallogenetic belt, its geologic condition is advantageous for the mineralization.
大悟县地处湖北省东北部，大别山脉西段，有着较丰富的旅游资源，但是尚未被有效开发。
Dawu county lies to the northeast of Hubei province and the west of Dabie mountains. Dawu county has rich tourism resources that have not been developed yet.
小独山西钨矿床位于塔里木板块的东端，北山陆缘活动带古生代柳园-俞井子裂谷带西段。
Xiaodushangxi tungsten deposit is located in the eastern end of the tarim plate, Beishan paleozoic continental margin activity with Liuyuan-Yu Well son with the western part of Rift Valley.
就目前研究状态而言。确定了早中泥盆世地层在东昆仑西段地区由西往东廷仲的位置。同时。
By the researching currently, the range of the Early-Middle Devonian strata ranging from west to east in west-middle section of east Kunlun Mt. is certained.
车路沟英安斑岩产于北祁连山西段，由大小不同的12个斑岩岩体组成，属于钙碱性系列岩石。
Located in the western part of North Qilian Mountains and composed of 12 small intrusions, Chelugou dacite porphyry shows petrochemically to be calialkelinic series.
在河西走廊西段酒西盆地中心偏北部的阴洼山西侧发现了南北走向的阴洼山西缘左行逆冲断裂。
A SN-trending left-slip thrusting active fault has been found at the western Yinwashan margin in north of Jiuxi basin, western segment of Hexi corridor.
冈底斯西段赛利普一带分布有大面积的钾质火山岩，以前曾被划归上新世一早更新世赛利普群。
Large area of potassic volcanic rocks distributed over the Sailipu area of West Gangdis were originally assigned to the Sailipu Group and the age was Pliocene-Early Pleistocene.
冈底斯西段赛利普一带分布有大面积的钾质火山岩，以前曾被划归上新世一早更新世赛利普群。
Large area of potassic volcanic rocks distributed over the Sailipu area of West Gangdis were originally assigned to the Sailipu Group and the age was Pliocene-Early Pleistocene.
应用推荐