地磁梯度测量及其在金属矿勘查中的试验——以拉依克勒克铜铁矿为例
王昊, 严加永, 孟贵祥, 吕庆田, 王栩

Geomagnetic gradient exploration and its test in metal deposits: a case study of the Layikeleke copper-iron deposit
Hao WANG, Jia-Yong YAN, Gui-Xiang MENG, Qing-Tian LU, Xv WANG
图1 东准噶尔拉伊克勒克矿区及周边地质[21]
Q—第四系;D2b1—中泥盆统第一岩性段;D2b2—中泥盆统第二岩性段; D 2 2 —中泥盆统安山岩; D 2 1 —中泥盆统玄武岩;D1t—下泥盆统托让格库都克组; γ 4 2 —海西期二长花岗岩;γ π 4 2 —海西期花岗斑岩;δ O 4 2 —海西期石英闪长岩;γ δ 4 2 —海西早期花岗闪长岩;γ ξ 3 2 —加里东期英云闪长岩;βμ—辉绿岩脉
Fig.1 Geological map of the Layikeleke ore district, Eastern Junggar[21]
Q—Quaternary; D2b1—First lithologic member of Middle Devonian; D2b2—Second lithologic member of Middle Devonian; D 2 2 —Middle Devonian andesite; D 2 1 —Middle Devonian basalt; D1t—Tuorangekuduke formation of Lower Devonian System; γ 4 2 —Hercynian monzonitic granite; γ π 4 2 —Hercynian granite porphyry; δ O 4 2 —Hercynian quartz diorite; γ δ 4 2 —early Hercynian granodiorite; γ ξ 3 2 —Caledonian tonalite; βμ—diabase dikes