1) Dahalajunshan formation
大哈拉军山组
1.
anthologic, petrographic and paleovolacanic apparatus study of volcanic and subvolcanic rocks of Dahalajunshan Formation in Axi mining district on the northern side of Ili basin, and study of paleovolcanic apparatus are conducted to probe into how gold deposits are controlled by paleovolcanic apparadus and sub-volcanic rock facies.
通过对盆地北缘阿希金矿区下石炭统大哈拉军山组火山岩、次火山岩岩石学、岩相学及古火山机体的详细研究，探讨了古火山机体和次火山岩相对金矿床的控制作用。
2.
The Yiarmand gold deposit occurs in hydrothermally eruptive breccia of the 2nd Member of Lower Carboniferous Dahalajunshan Formation and its underlying arsenopyritized and pyritized tuffaceous clastic rocks,and the ore forming process can be divided into hydrothermally eruptive and sedimentary stage and metasomatic stage.
伊尔曼德金矿床赋存于下石炭统大哈拉军山组第二岩性段硅化热液喷发角砾岩及其下伏上泥盆统吐呼拉苏组毒砂黄铁矿化凝灰质碎屑岩中，成矿作用可分为热液喷发沉积期和热液交代蚀变成矿期。
3.
The early Carboniferous Saikendulu series and Dahalajunshan Formation volcanic rocks are similar studied by petrochemistry ,trace element and REE,.
岩石化学和元素地球化学研究表明,早石炭世赛肯都鲁序列和大哈拉军山组火山岩具有相似性,两者SiO2含量平均值分别为62。
2) Dahalajunshan group
大哈拉军山组
1.
Tuhulasu gold deposit is included in silicated conglomerate, Silicated tuffaceous conglomerate、pyritized silieic tuff of Dahalajunshan group of lower carboniferous.
吐呼拉苏金矿床赋存于下石炭统大哈拉军山组底部的硅化凝灰质砾岩、硅化砾岩、黄铁矿化酸性凝灰岩中。
4) the background of the formation of Dahala Junshan volcanic rock
大哈拉军山火山岩系形成背景
5) Halahatang Formation
哈拉哈塘组
1.
Forming Mechanism of Hydrocarbon Reservoirs of Halahatang Formation in Yuqi Block in Akekule Arch,Tarim Basin;
塔里木盆地阿克库勒凸起于奇地区哈拉哈塘组油气成藏机制
2.
The characteristics and influential factors of Halahatang Formation reservoir in Yuqi area,Akekule uplift are studied by means of core inspection,casting thin section,cathodology,SEM,porosity and permeability analysis,mercury intrusion method etc,hydrocarbon charge and accumulation law are studied with the technologies,such as fluorescence thin section and fluid inclusion.
利用岩芯观测、铸体薄片、阴极发光、扫描电镜、物性分析、压汞等方法,总结了于奇地区哈拉哈塘组储层特征及影响因素;应用荧光薄片与流体包裹体分析等技术和方法,综合研究了油气注入史与成藏规律。
6) Hala'alat mountain
哈拉阿拉特山
1.
The Hala'alat mountain,the eastern segment of the leading thrust belt,is composed of four elements such as Xiemisitai monocline,the Heshituologai basin,the Hala'alat imbricated zone and the western slope of Mahu sag.
准噶尔盆地西北缘前陆冲断带是自石炭纪晚期发育起来的大型叠瓦冲断系统,哈拉阿拉特山冲断带为其冲断前锋构造带的东段。
补充资料：军都山
北京市主要山脉。位于市区以北，昌平、延庆、怀柔县境，处太行山与燕山交接部。形成于中生代燕山运动，以褶皱、断层构造为主，并有岩浆侵入，花岗岩等岩浆岩和古老变质岩广布。西南-东北走向，重峦叠嶂，主要山峰如黑坨山、凤坨梁等，海拔1500米以上。山名疑源于古代部落桓都，亦作浑都，后演变为军都。又名南口山。温榆河发源其阳，白河横穿其阴。居庸关位其西翼，古北口控其东陲，军事和交通地位重要。山南麓有明"十三陵"。长城蛇形于山脊沟壑，气势磅礴，蔚为壮观,尤以八达岭、慕田峪等地段保存完好,为世界驰名的游览胜地。明代山上森林仍称茂密，后遭破坏。现南口、十三陵、密云水库（见密云县）周围和延庆县刘斌堡至四海冶一带，天然次生林和人工林生长良好，为北京市重要植林地区。
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参考词条