滇西北兰坪盆地金满脉状铜矿床成矿流体特征及其成矿意义
Ore-Forming Fluid Characteristics of the Jinman Vein-Type Copper Deposits in the Western Lanping Basin and Its Metallogenic Significance
查看参考文献43篇
|
文摘
|
滇西北兰坪盆地西缘发育大量沉积岩容矿脉状铜多金属矿床,矿体的分布受逆冲推覆系统控制,金满是其中储量最大、品位最高的铜矿床。成矿过程可分为3个阶段:成矿前(不含矿化石英-铁白云石脉)、主成矿阶段(含铜硫化物石英脉)、晚成矿阶段(少硫化物方解石+石英脉)。流体包裹体岩相学和显微测温结果表明:成矿前和主成矿期石英中流体包裹体特征变化不大,成矿前和主成矿期石英中均存在3种类型的包裹体,以水溶液包裹体为主,含CO_2水溶液包裹体次之,富CO_2包裹体较少出现。含CO_2水溶液包裹体测温结果也差别不大,均一温度都集中在240320℃,盐度(w(NaCl))集中在1%4%。水溶液包裹体均一温度变化也不大,集中在160 230℃,明显低于含CO_2水溶液包裹体;盐度却存在较大的变化,主成矿期盐度变化范围明显较大,且峰值高于成矿前。晚成矿阶段则仅出现水溶液包裹体,均一温度和盐度都明显降低,均一温度集中在120185℃,盐度集中在1.4%9.3%。结合其他证据,笔者认为金满铜矿床包含两种不同性质的流体:深源流体,以中高温、中低盐度、富含CO_2为特征;盆地卤水,以中低温、中高盐度、贫CO_2为特征。成矿过程中未发生明显的沸腾和相分离作用,深源流体和盆地卤水的混合可能是导致Cu等成矿元素沉淀的重要机制。 |
|
其他语种文摘
|
A large number of sediment-hosted vein-type copper deposits controlled by a thrust-nappe system have been discovered in the west part of the Lanping basin,among which,the Jinman deposit is the largest in tonnage scale and with the highest Cu grade.The mineralization process of this deposit can be divided into three stages,including the early stage(pre-ore quartz-ankerite vein stage),the major stage(massive polymetallic sulphide-quartz vein stage),and the late stage(carbonate-quartz stage). The detailed studies of fluid inclusions distinguishes three types of fluid inclusions dominated by aqueous water in both pre-ore and syn-ore quartz from the Jinman deposit,including aqueous water,CO_2- bearing,and pure CO_2inclusions.There is no obvoius difference between pre-ore and syn-ore quartz in terms of the type of fluid inclusions and microthermometric parameters of their CO_2-bearing inclusions. The homogenization temperatures of CO_2-bearing inclusions in both pre-ore and syn-ore quartz vary from 217to 334 ℃(peak at 240320 ℃),with corresponding salinities ranging from 1%to 4%.The homogenization temperatures of aqueous inclusions in both pre-ore and syn-ore quartz vary from 143℃ to 239℃(peak at 160230℃),much lower than those of CO_2-bearing inclusions.However,the salinities of aqueous inclusions show significant difference between pre-ore(3.1%18.0%)and syn-ore quartz(4.1%22.8%).Quartz-calcite vein in the late mineralizing stage only have aqueous inclusions,with homogenization temperature of 120185 ℃,and salinities of 1.4%9.3%.The fluid inclusion characteristics,together with other evidence,indicate that(1)there are two fluid systems responsible for Cu mineralization in the Jinman deposit one is deep crustal fluids,characterized by high CO_2content and relatively low salinities,and the other is basin brine,characterized by relatively high salinities and low temperatures.(2)The fluid mixing,without boiling or phase separation,might be the major precipitation mechanism. |
|
来源
|
吉林大学学报. 地球科学版
,2017,47(3):706-718 【核心库】
|
|
DOI
|
10.13278/j.cnki.jjuese.201703106
|
|
关键词
|
成矿流体
;
沉积岩容矿脉状铜矿床
;
金满脉状铜矿床
;
兰坪盆地
|
|
地址
|
1.
中国地质调查局成都地质调查中心, 成都, 610081
2.
中国科学院地球化学研究所, 贵阳, 550002
3.
成都理工大学地球科学学院, 成都, 610059
|
|
语种
|
中文 |
|
文献类型
|
研究性论文 |
|
ISSN
|
1671-5888 |
|
学科
|
地质学 |
|
基金
|
国家自然科学基金青年科学基金项目
;
国土资源部中国地质调查局地质调查项目
|
|
文献收藏号
|
CSCD:5996492
|
参考文献 共
43
共3页
|
|
1.
薛春纪. 滇西兰坪盆地构造体制和成矿背景分析.
矿床地质,2002,21(1):36-44
|
被引
68
次
|
|
|
|
|
2.
侯增谦. 青藏高原碰撞造山带Pb—Zn—Ag—Cu矿床新类型：成矿基本特征与构造控矿模型.
矿床地质,2008,27(2):123-144
|
被引
97
次
|
|
|
|
|
3.
He Longqing. Thrust-Controlled,Sediment-Hosted,Himalayan Zn-Pb-Cu-Ag Deposits in the Lanping Foreland Fold Belt, Eastern Margin of Tibetan Plateau.
Ore Geology Reviews,2009,36:106-132
|
被引
51
次
|
|
|
|
|
4.
邓军. 三江特提斯复合造山与成矿作用.
矿床地质,2010,29(1):37-42
|
被引
124
次
|
|
|
|
|
5.
宋玉财. “三江"喜马拉雅期沉积岩容矿贱金属矿床基本特征与成因类型.
岩石矿物学杂志,2011,30(3):355-380
|
被引
60
次
|
|
|
|
|
6.
Misra K C.
Understanding Mineral Deposits,2000
|
被引
11
次
|
|
|
|
|
7.
侯增谦. 青藏高原碰撞造山带:Ⅱ.晚碰撞转换成矿作用.
矿床地质,2006,25(5):521-543
|
被引
262
次
|
|
|
|
|
8.
何明勤.
兰坪盆地铅锌铜大型矿集区的流体成矿作用机制:以白秧坪铜钴多金属地区为例,2004
|
被引
3
次
|
|
|
|
|
9.
李峰.
滇西红层铜矿地质,2000
|
被引
4
次
|
|
|
|
|
10.
王光辉.
滇西兰坪盆地金满-连城脉状铜矿床成因研究,2010
|
被引
2
次
|
|
|
|
|
11.
胡瑞忠. 金顶超大型铅-锌矿床氦、氩同位素地球化学.
中国科学:D辑,1998,28(3):208-213
|
被引
48
次
|
|
|
|
|
12.
薛春纪. 滇西北兰坪铅锌银铜矿田含烃富CO_2成矿流体及其地质意义.
地质学报,2002,76(2):244-253
|
被引
47
次
|
|
|
|
|
13.
赵海滨.
滇西兰坪盆地中北部铜多金属矿床成矿地质特征及地质条件,2006
|
被引
6
次
|
|
|
|
|
14.
Chi Guoxiang. Abundance of CO_2-Rich Fluid Inclusions in a Sedimentary Basin-Hosted Cu Deposit at Jinman,Yunnan,China:Implications for Mineralization Environment and Classification of the Deposit.
Mineralium Deposita,2011,46:365-380
|
被引
20
次
|
|
|
|
|
15.
Xue Chunji. Geologic, Fluid Inclusion and Isotopic Characteristics of the Jinding Zn-Pb Deposit,Western Yunnan,South China:A Review.
Ore Geology Reviews,2007,31:337-359
|
被引
92
次
|
|
|
|
|
16.
刘家军. 兰坪—思茅盆地砂页岩中铜矿床同位素地球化学.
矿床地质,2000,19(3):223-234
|
被引
42
次
|
|
|
|
|
17.
吴南平. 云南兰坪-思茅盆地脉状铜矿床铅、硫同位素地球化学与成矿物质来源研究.
岩石学报,2003,19(4):799-807
|
被引
33
次
|
|
|
|
|
18.
Ji Hongbing. Geochemistry of Jinman Copper Vein Deposit, West Yunnan Province, China: Ⅱ: Fluid Inclusion and Stable Isotope Geochemical Characteristics.
Chinese J Geochemy,1998,17(1):81-90
|
被引
8
次
|
|
|
|
|
19.
阙梅英.
兰坪-思茅盆地铜矿床,1998
|
被引
6
次
|
|
|
|
|
20.
何明勤. 云南兰坪金满铜矿床改造成因的证据.
地质与勘探,1998,34(2):13-15
|
被引
14
次
|
|
|
|
|
了解气象卫星更多信息，请访问