2) epigenetic hydrothermal metallization
后生热液成矿
1.
Two mineralization stages has been distinguished, one is Mesoproterozoic Palaezoic syndepositional mineralization in sea basins, the other is Mesozoic epigenetic hydrothermal metallization in the int.
指出区内总体成矿地质背景为具有过渡型地壳特色的大陆复合型造山带 ,可划分为中元古代-古生代海盆同生沉积成矿、中生代大规模陆内俯冲造山体制后生热液成矿两个成矿阶段 ,具有盆地边缘控矿、动力学转换带成矿、成矿的广义层控性及碰撞造山体制浅成与中深成热液矿带成对共生等特
3) By solution and hydrothermal reactions
溶液和水热条件
4) ore-forming fluid
成矿溶液
1.
The characteristics of stable isotope indicatedthat the ore-forming material was leached from the wall rocks ;and the ore-forming fluid wasmainly supplied by meteoric water.
稳定同位素特征揭示了矿质来说从围岩中淋取；成矿溶液主要来源于大气降水。
5) Demineralization solutions
脱矿溶液
补充资料：和表
1.即华表。古代陵墓﹑宫殿等前所立的表柱。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条