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作 者:宋忠宝[1] 杨合群[1] 谢春林[1] 李新科[2] 栗亚芝[1] 王兴安[1] 李文明[1] 李长安[1]
机构地区:[1]西安地质矿产研究所,陕西西安710054 [2]陕西地勘局物化探队,陕西西安710400
出 处:《西北地质》2006年第3期1-6,共6页Northwestern Geology
基 金:中国地质调查局地质调查项目"北祁连山错沟-寺大隆一带铜矿预查评价"(编号:200110200152);国土资源部资源补偿费项目"甘肃省肃南裕固族自治县雪泉铜(锌)矿普查"(编号:中地调发[2003]18号)资助
摘 要:通过对石居里一带岩矿石物性测量,可知块状矿石视极化率最高,视电阻率最小,为明显低阻高极化显示。碳质板岩、网脉状矿石、含矿碧玉岩视极化率次之,视极化率6%~9%,视电阻率较高。其余硅质岩、碧玉岩、细碧岩、凝灰质砂岩为高阻低极化,视极化率一般在1%~3%。由物性参数看出,该区实施激电测量,寻找铜硫化物矿产的物性前提是具备的。碧玉岩磁化率为最高,变化值在1030×4π×10-6SI^17515×4π×10-6SI,平均值达4521×4π×10-6SI,次为细碧岩、凝灰质砂岩,磁化率平均为1000×4π×10-6SI,~2000×4π×10-6SI左右,其余碳质板岩、硅质岩、次生石英岩、不纯碧玉岩、矿石均为弱磁性,在几十至几百之间变化。由于矿体与碧玉岩紧密相关,且高纯度的碧玉岩更是比其他岩性见矿率高,故对于以碧玉岩为标志,以磁性寻找碧玉岩以达到间接找矿,物性前提是具备的。The geophysical exploration in the Shijuli area has determined that the massive ores have the highest apparent chargeability and the lowest apparent resistivity. The apparent chargeability of 6%~9% for carbon-bearing slates, reticulated ores and ore-bearing jaspilites is lower than massive ores, but the apparent resistivity is higher. The other rocks, such as silicalite, jaspilite, spilite, tuffaceous sandstone, show high resistivity and low chargeability (1%~3%) in nature. These geophysical parameters indicate that conditions are available in this areas for prospecting copper sulfide deposit using induced polarization method. Susceptibility of Jaspilite is the highest (1 030~17 515) and the mean is 4 521×4π×10 -6SI, the follows are spilite and tuffaceous sandstone,their mean susceptibility is 1 000×4π×10 -6SI^2 000×4π×10 -6SI, the other ricks,such as anthrinoid slates, silicalite,secondary quartzites, impure jaspilites and ores,have weak magnetism,varied from several decades to hundreds.As the orebody is very close to jaspilites while the ores are found more often in the high-pure jaspilites than in other rocks. By its higher susceptibility, jaspilite is excellent indication to prospect copper deposit.
关 键 词:视极化率 视电阻率 塞浦路斯型块状硫化物矿床 石居里 北祁连山
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