云南地质
雲南地質
운남지질
YUNNAN GEOLOGY
2011年
3期
316-320
,共5页
裂谷早期%裂堑盆地%生长断层%碱基性火山喷发%喷溢热水沉积成矿
裂穀早期%裂塹盆地%生長斷層%堿基性火山噴髮%噴溢熱水沉積成礦
렬곡조기%렬참분지%생장단층%감기성화산분발%분일열수침적성광
Earlier Period of Rift%Graben Basin%Growth Fault%Alkaline - Basic Volcanic Eruption%Ef-fusive Hydrothermal Sedimentary Metallogenesis
落因背斜两翼地层构造、地层岩相、含矿的差异性，证明背斜轴部存在生长断层。凡有长断层出现，因民组、落雪组岩相剧变，伴随碱性火山喷发一喷溢活动形成细碧岩、基性熔岩、角砾岩之处成为成矿必要条件。
落因揹斜兩翼地層構造、地層巖相、含礦的差異性，證明揹斜軸部存在生長斷層。凡有長斷層齣現，因民組、落雪組巖相劇變，伴隨堿性火山噴髮一噴溢活動形成細碧巖、基性鎔巖、角礫巖之處成為成礦必要條件。
락인배사량익지층구조、지층암상、함광적차이성，증명배사축부존재생장단층。범유장단층출현，인민조、락설조암상극변，반수감성화산분발일분일활동형성세벽암、기성용암、각력암지처성위성광필요조건。
The differences in strata, structure, rock facies and ore - bearing of two limbs of Luo - Yin anti- cline prove that there is the fauh in the anticlinal axis. The necessary conditions of metallogenesis are appearance of growth fault; intense variation of Yinmin Formation, Luoxue Formation rock facies; the places of forming spilite, basic lava, breccia.
