1) Daheigou
大黑沟
1.
Studies on Mineral Elements for Cultivated Rheum in Daheigou, Qinghai Province;
青海省大黑沟种植大黄中矿物质元素研究
2) Heigou Fault
黑沟大断裂
1.
Based on the measurements of the vertical and lateral breaks of the terraces of Laoguanhe River, it is found that Heigou Fault had a strong activation since middle of Late Pleistocene epoch.
通过对老灌河河流阶地水平错断幅度和垂直错断幅度的测量 ,证实自晚更新世中期以来黑沟大断裂的构造活动十分强烈 ,主要表现为水平方向上的大规模左旋走滑活动 ,在垂直方向上的活动相对来说比较微弱。
3) Heigou large deep fault
黑沟深大断裂
4) Heishigou bridge
黑石沟特大桥
1.
Labajin and Heishigou bridge are the composite structure of long span continuous rigid frame with high-frusta concrete and con- crete-filled steel tube projects,the height of the major frusta of these two bridges are 182.
腊八斤特大桥、黑石沟特大桥为大跨连续刚构钢管混凝土组合高墩混凝土工程,其主墩最高墩高分别为182。
5) Heishuigou-Dashujiao ore area
黑水沟-大树脚矿区
6) Heicigou
黑刺沟
1.
Gold mineralization related to quartze monzonite diorite in Heicigou area of Danghe Nanshan;
党河南山黑刺沟地区与石英二长闪长岩有关的金矿化
2.
In order to study the metallogenic regularity and gold and copper ore_control factors on the northern slope of Danghenanshan area in South Qilian Mountains, the authors made a systematical geological and geochemical studies on the Heicigou and the Jiagongtai gold deposits in this area.
为深入研究甘肃南祁连党河南山北坡金铜矿产的成矿规律和控矿因素 ,笔者采用地质地球化学方法首次对区内黑刺沟和贾公台两个金矿床进行了较为系统的研究 ,发现它们的成矿特征有很大差异 :黑刺沟金矿床以富As,Sb的微细浸染蚀变岩型金矿化为主 ,其次为辉锑矿石英脉型金矿化 ;而贾公台金矿床则以少硫化物石英脉型金矿化和蚀变岩型金矿化为特征 ,As,Sb含量不高。
