1) biogenic and epigenetic ore deposit
生物后生成矿
2) epigenetic mineralization
后生成矿
1.
Evidences of the epigenetic mineralization processand geochemical features of Mujiazhuang copper deposit;
陕西穆家庄铜矿床后生成矿作用的流体地球化学证据
3) biomineralization
生物成矿
1.
Research of biomineralization has had a long history, but the function of living beings and organic evolution in mineralization was usually ignored.
生物成矿研究由来已久 ,但生物及其有机质演化在成矿中的作用长期得不到应有的重视。
2.
According to the relationship between biomineralizations and living things, there are two kinds of biominerali zations: the biologic ally induced mineraliza.
细菌在水系中普遍存在并具有固有的生物成矿能力 ,因此 ,它们在控制现代和古代沉积环境中铁的循环起到极为重要的作用。
4) Bio mineralization
成矿生物
5) Microbial Biomineralization
微生物成矿
6) 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
补充资料：后生仔
1.见"后生子"。
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