Lamprophyres

基本解釋

Lamprophyres in the orefield may be divided into tow groups fresh (weak alteration)and altered.
根據(jù)巖石的蝕變相對(duì)強(qiáng)弱，本區(qū)煌斑巖可分成新鮮（弱蝕變）、蝕變兩種。
The lamprophyres are widely distributed in Qinling, which are mostly well auriferous.The lamprophyres are occurred in silty slates of Palaezoic Silurian and Devonian systems.
秦嶺地區(qū)廣泛分布有煌斑巖，其主要賦存于古生界志留系與泥盆系的粉砂質(zhì)板巖中，大部分含金較高。
Lamprophyres in the Taoyuan-Xiaotongjiapuzi gold ore belt is of strong enrichment type of incompatible elements, with obvious fractionation among incompatible elements.
桃源-小佟家堡子金礦帶煌斑巖為不相容元素強(qiáng)烈富集型，不相容元素間分餾明顯，高場(chǎng)強(qiáng)元素豐度較低，低場(chǎng)強(qiáng)元素豐度較高。
According to the contrast study on the relations between lamprophyre and gold mineralization, it indicates that there are simularities between the lamprophyres.
經(jīng)不同成礦區(qū)煌斑巖與金礦成礦關(guān)系的對(duì)比研究，認(rèn)為其具有相似性，并與金成礦關(guān)系密切。
Keywords gold deposits;lamprophyres;petrochemistry;Yunnan;
金礦床;煌斑巖;巖石化學(xué);云南;