黄金
黃金
황금
GOLD JOURNAL
2013年
9期
11-15
,共5页
店房金矿床%稳定同位素%成矿示踪%河南嵩县
店房金礦床%穩定同位素%成礦示蹤%河南嵩縣
점방금광상%은정동위소%성광시종%하남숭현
Dianfang gold deposit%stable isotope%metallogenesis tracing%Song County,Henan Province
店房金矿床位于河南嵩县,经过勘探,提交金金属量12.62 t,伴生铅金属量26370 t,银金属量153.16 t。矿区δ34 S值为3.4‰~5.9‰,离散程度小,表明经过了均一化过程,也说明成矿物质是地幔和下地壳混合来源;铅同位素变化较小,206 Pb/204 Pb为16.9314~17.4121,207 Pb/204 Pb为15.1607~15.1753,208 Pb/204 Pb为37.3210~38.7644,铅同位素研究显示成矿铅来自地幔和下地壳,结合构造通道和矿体形态研究,可以预测在矿区爆破角砾岩外围东南深部存在隐伏岩体;矿区硫同位素显示,矿体中方铅矿δ34 S、近矿围岩方铅矿δ34 S、远矿围岩δ34 S具有不同特征,通过对钻探岩芯中方铅矿δ34 S测试可以为深部找矿勘探提供依据。
店房金礦床位于河南嵩縣,經過勘探,提交金金屬量12.62 t,伴生鉛金屬量26370 t,銀金屬量153.16 t。礦區δ34 S值為3.4‰~5.9‰,離散程度小,錶明經過瞭均一化過程,也說明成礦物質是地幔和下地殼混閤來源;鉛同位素變化較小,206 Pb/204 Pb為16.9314~17.4121,207 Pb/204 Pb為15.1607~15.1753,208 Pb/204 Pb為37.3210~38.7644,鉛同位素研究顯示成礦鉛來自地幔和下地殼,結閤構造通道和礦體形態研究,可以預測在礦區爆破角礫巖外圍東南深部存在隱伏巖體;礦區硫同位素顯示,礦體中方鉛礦δ34 S、近礦圍巖方鉛礦δ34 S、遠礦圍巖δ34 S具有不同特徵,通過對鑽探巖芯中方鉛礦δ34 S測試可以為深部找礦勘探提供依據。
점방금광상위우하남숭현,경과감탐,제교금금속량12.62 t,반생연금속량26370 t,은금속량153.16 t。광구δ34 S치위3.4‰~5.9‰,리산정도소,표명경과료균일화과정,야설명성광물질시지만화하지각혼합래원;연동위소변화교소,206 Pb/204 Pb위16.9314~17.4121,207 Pb/204 Pb위15.1607~15.1753,208 Pb/204 Pb위37.3210~38.7644,연동위소연구현시성광연래자지만화하지각,결합구조통도화광체형태연구,가이예측재광구폭파각력암외위동남심부존재은복암체;광구류동위소현시,광체중방연광δ34 S、근광위암방연광δ34 S、원광위암δ34 S구유불동특정,통과대찬탐암심중방연광δ34 S측시가이위심부조광감탐제공의거。
Dianfang gold deposit is located in Song County ,Henan,with exploration submitting metal quantity of gold 12.62 t,of lead 26 370 t and of silver 153.16 t.The value of δ 34 S is 3.4-5.9 in ore district,and its assembling characteristics prove that it came through homogenization process ,and that the source is a mixture of things consisting of the mantle and the lower crust;Changes of Pb isotope are relatively small ,with 206 Pb/204 Pb:16.9314-17.4121, 207 Pb/204 Pb:15.1607-15.1753,and 208 Pb/204 Pb:37.3210-38.7644.Pb isotope shows metallogenic lead came from the mantle and lower crust , and by studying geological structure and Pb isotope , hidden ore bodies in the southeast deep part of cryptoexplosive breccia peripherals can be predicted .the δ34 S of galena shows different characteristics of ore bodies from that of near wall rocks and far wall rocks .it can offer evidence for exploration in the deep part of de-posits by testing δ34 S of galena in the drill core .