北祁连山石居里一带塞浦路斯型铜矿床岩矿石物性特征

宋忠宝, 杨合群, 谢春林, 李新科, 栗亚芝, 王兴安, 李文明, 李长安. 北祁连山石居里一带塞浦路斯型铜矿床岩矿石物性特征[J]. 西北地质, 2006, 39(3): 1-6.
引用本文: 宋忠宝, 杨合群, 谢春林, 李新科, 栗亚芝, 王兴安, 李文明, 李长安. 北祁连山石居里一带塞浦路斯型铜矿床岩矿石物性特征[J]. 西北地质, 2006, 39(3): 1-6.
SONG Zhong-bao, YANG He-qun, XIE Chun-lin, LI Xin-ke, Li Ya-zhi, Wang Xing-an, LI Wen-ming, LI Chang-an. Physical Properties of Rocks and Ores Associated with Shijuli Cyprus-Type Copper-Rich Massive Sulfide Deposit in North Qilian Mountains[J]. Northwestern Geology, 2006, 39(3): 1-6.
Citation: SONG Zhong-bao, YANG He-qun, XIE Chun-lin, LI Xin-ke, Li Ya-zhi, Wang Xing-an, LI Wen-ming, LI Chang-an. Physical Properties of Rocks and Ores Associated with Shijuli Cyprus-Type Copper-Rich Massive Sulfide Deposit in North Qilian Mountains[J]. Northwestern Geology, 2006, 39(3): 1-6.

北祁连山石居里一带塞浦路斯型铜矿床岩矿石物性特征

  • 基金项目: 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

Physical Properties of Rocks and Ores Associated with Shijuli Cyprus-Type Copper-Rich Massive Sulfide Deposit in North Qilian Mountains

  • 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。
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出版历程
收稿日期:  2005-06-20
修回日期:  2005-11-18
刊出日期:  2006-09-15

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