印度尼西亚西加里曼丹省卡普阿斯河下游地区锆英石成矿规律研究
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摘要
加里曼丹岛位于西太平洋东南亚陆缘构造岩岩浆活动带,是自中新生代以来地球岩石圈最复杂的构造活动区之一,研究区有很好的成矿前景。本文研究目的是对矿床的物质来源,成矿环境和成矿作用进行讨论,总结锆英石在该区的成矿规律,为在该地区寻找大而富的锆英石砂矿资源提供依据。
本文先是对含矿地层进行了划分,又从水平方向上和垂直方向上对该区的含矿地层进行比较和研究,再根据搜集资料和项目的勘探实际成果数据分析验证。
研究发现,该矿床为一大型的冲积型的砂矿床,矿体赋存于第四系地层中；石英砂矿在全区分布较广泛,锆英石的成矿受阶地控制；锆英石的物源主要是花岗闪长岩等侵入岩；该研究区的锆英石砂矿以石英、长石、钛铁矿、磁铁矿、锆英石、砂金等为主,其次为金红石、独居石。砂矿的分布与物源基岩性质、地貌、水系、动力条件、气候、等密切相关；最后将卡普阿斯河中上游地区划为成矿远景区。
Kalimantan Island is located in the southeastern Asian continental marginal tectono-magmatic mobile zone in the Western Pacific Ocean, where the Earth's lithosphere is one of the most complicated tectonic mobile region in the earth since the Meso-Cenozoic. Study areas have very good metallogenic prospects. This study aims to discuss the deposit source material, environmental and mineralization of metallogenic, sums up ore-forming regularity of Zirconite in the region, and be the base of looking for big and rich Zirconite mineral resources.
At first, we divide the, and compare the ore containing formation from the horizontal and vertical direction, and then, analysis according to data collection and exploration result.
After the study, I found the deposit is a large-scale alluvial sand deposit, and the ore body exists in the Q stratum; There is large distribution of the quartz sand placer in the whole region, and the distribution of Zircon placer layer is controlled by the terrace. The main material source of Zircon are granodiorite intrusive rocks, etc; Most of the alluvial Zircon sand resource in this region exists in terraces and convex bank of Kapuas River; At last, I summarize the distribution law of the deposit horizontally and vertically, and predict the region upper Kapuas River will be resource prospect area.
本文先是对含矿地层进行了划分,又从水平方向上和垂直方向上对该区的含矿地层进行比较和研究,再根据搜集资料和项目的勘探实际成果数据分析验证。
研究发现,该矿床为一大型的冲积型的砂矿床,矿体赋存于第四系地层中；石英砂矿在全区分布较广泛,锆英石的成矿受阶地控制；锆英石的物源主要是花岗闪长岩等侵入岩；该研究区的锆英石砂矿以石英、长石、钛铁矿、磁铁矿、锆英石、砂金等为主,其次为金红石、独居石。砂矿的分布与物源基岩性质、地貌、水系、动力条件、气候、等密切相关；最后将卡普阿斯河中上游地区划为成矿远景区。
Kalimantan Island is located in the southeastern Asian continental marginal tectono-magmatic mobile zone in the Western Pacific Ocean, where the Earth's lithosphere is one of the most complicated tectonic mobile region in the earth since the Meso-Cenozoic. Study areas have very good metallogenic prospects. This study aims to discuss the deposit source material, environmental and mineralization of metallogenic, sums up ore-forming regularity of Zirconite in the region, and be the base of looking for big and rich Zirconite mineral resources.
At first, we divide the, and compare the ore containing formation from the horizontal and vertical direction, and then, analysis according to data collection and exploration result.
After the study, I found the deposit is a large-scale alluvial sand deposit, and the ore body exists in the Q stratum; There is large distribution of the quartz sand placer in the whole region, and the distribution of Zircon placer layer is controlled by the terrace. The main material source of Zircon are granodiorite intrusive rocks, etc; Most of the alluvial Zircon sand resource in this region exists in terraces and convex bank of Kapuas River; At last, I summarize the distribution law of the deposit horizontally and vertically, and predict the region upper Kapuas River will be resource prospect area.
引文
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6 阙薇,攀西地区钛砂矿成矿条件及成矿远景,矿物岩石地球化学通报,283-285；
7 刘英俊,勘查地球化学,北京,科学出版社,1987；
8 阙薇,攀西地区钛砂矿成矿条件及成矿远景,矿物岩石地球化学通报,283-285；
9 王中波,长江水系沉积物碎屑矿物组成及其示踪意义,沉积学报,2006(24),570-578；
10 赵红格,物源分析方法和研究进展,沉积学报,2003,21(3)：409-415；
11 吕全荣,长江口细颗粒沉积物的矿物特征和沉积分异.上海地质,1992,43(3)：18-25；
12 赵财胜,西南太平洋区域地质、成矿作用及Punda金铜矿床特征研究,长春：吉林大学,2002；
13 卫敏,印度尼西亚桑义赫岛海滨砂矿可选性试验研究,矿产保护与利用,2009(2),33-36；
14 裴荣富,特大型矿床研究若干问题探讨,中国地质,2001(7),9-15；
15 朱章显,苏拉威西埃达克岩、类埃达克岩分布与特征,吉林大学学报,2009(39)；
16 丁清峰,东南亚北加里曼丹新生代碰撞造山带演化与成矿[J].吉林大学学报：地球科学版,2004,34(2),193-200；
17 周蒂,南沙海区及邻区构造演化动力学的若干问题[J].大地构造与成矿学,2005,29(3)：339-345；
18 郭依辉,南沙海域东南部地形地貌特征,南沙海域东南部地质地球物理综合研究专辑,武汉,中国地质大学出版社,1996,26-39；
19 吕新彪,长江中下游地区地质异常与成矿,地质学报,1998,72(3)：260-266；
20 薛君治,成因矿物学,武汉：地质出版社,1986.23-35；
21 孙玉波.1982,重力选矿.北京：冶金工业出版社；
22 高树学,2006,黑龙江省桦南砂金矿区砂金成矿物质来源及成因,采矿技术,Vol.6 No.3,591-593;
23 虞平,2007,近两年我国锆英砂及其精矿进口情况分析,市场分析与预测,Vol.26,No.8,20-24：
24 吕英杰,1988,辽宁、吉林、黑龙江地区流水成因的砂金矿,中国地质科学院院报,(18)70-90;
25 唐鑫,从板块构造观点论南海的成因1地球物理学报,1981,24(4)
26 万平益,巴山锰矿带地质特征、矿床成因及成矿远景分析,中国锰业,四川省冶金地质勘查局六O四大队；
27 阙薇,2008,攀枝花市钛砂矿成矿远景预测,No1,61-62；
28 方念乔,印度尼西亚多岛海沉积记录基本特征与云南古特提斯研究,地学前缘,2002,Vol9,No.3,79-87；
29 D.E考克斯、D.A.辛格,1986(宋伯庆等,1990译),矿床模式,地质出版社,33-44；
30 王昆山,长江水下三角洲沉积物的重矿物分布及组合,海洋地质与第四纪地质,2007(27)7-12
31 丁清峰,东南亚北加里曼丹新生代碰撞造山带演化与成矿,2004(34)：193-200；
32 王昆山,长江水下三角洲沉积物的重矿物分布及组合,海洋地质与第四纪地质,2007(27),8-12;
33 林晓彤等黄河物源碎屑沉积物的重矿物特征,海洋地质与第四纪地质,2003,23(3)：17-21；
34地矿部海洋地质研究所,中国的海洋砂矿,中国地质,1998(4)23-26；
35 王正铤,中国滨海砂矿成矿带,中国地质科学院天津地质扩产研究所所刊,1988(20)114-126：
36 杨森楠,中、新生代太平洋陆缘带的构造格局和构造转换,地学前缘(中国地质大学,北京),1997(4)247-255；
37 张宝柱,印度尼西亚地质矿产考察报告云南地质科技情报论文,云南地质科技情报,62-74；
38 王鸿祯,中国东部及邻区中、新生代盆地发育及大陆边缘区的构造发展,地质学报,1983,57(2)：213-223
39 殷鸿福等,中国古生物地理学1武汉：中国地质大学出版社,1988；
40 涂怀奎,冲积型金刚石砂矿与其成矿模式的讨论,化工矿产地质,2001(23)239-244；
41 沈若慧,台湾海峡西部海底有用重砂高品位分布与找矿意义,台湾海峡,1999(18),131-138：
42 李旭,加里曼丹及邻区壳体的运动与演化,大地构造与成矿学,2002(9)235-239；
43 Morton A and Hurst A. Correlation of sandstones using heavy minerals:an examp le from the Statfjord Formation of the Snorre Field, northern North Sea. In:Dunay R E, Hailwood E A, eds. Nonbiostrati-graphicalMethods of Dating and Correlation. Geological Society Special Publication,1995,89:3-22.
44 Duan Chenglong. An Analysis and Evaluation for the Situation of Titanium Resources. Sichuan Nonferrous metals,2000(2):31-34;
45 Pakiser L C, Zietz I. Transcontinental crust and upper mantle structure. Revs Geophys, 1965, (3):505-520;
46 Livaccari R F. Role of crustal thickening and extensional collapse in the tectonic evolution of the Sevier-Laramide orogeny western United States. Geol,1991,19(11): 1104-1107;
47 Jones D L, Cox A, Coney P, Beck M. The growth of western North America.Scientific American,1982,247(5):70-84;
48 Runcorn S K. Satellite gravity measurements and liminar viscous flow model of the Earth's mantle, J Geophys Res,1976(14):375-384;
49 Kaula W M. Global gravity and mantle convection. Tectonophysics,1972,13:341-359;
50 Tonkin P C, Himawan R. Basement lithology and its control on sedimentation, trap formation, hydrocarbon migration in Widuri-Intan oilfields, SE Sumatra[J].Journal of-Petroleum Geology,1999,22(2):141-165;
51 Howells C. Tertiary response to oblique subduction and indentation in Sumatra, Indonesia:New ideas for hydrocarbon exploration. Petroleum Geology of Southeast Asia:Geological society special publication,1997,126:365-374;
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2 叶金镜,2006,广东省西南沿海滨海砂矿成矿地质条件浅析,西部探矿工程,P744.2；239-240；
3 王占岐,1998,海滨砂矿中金红石矿综合利用研究,地球科学——中国地质大学学报,第23卷第6期,624-627；
4 王常任,1986,磁电选矿,第一版,北京：冶金工业出版社：49-51；
5 王宁,2002,海南残坡积砂矿采选工艺研究及环保对策,西南科技大学学报,Vol.17No.4,55-58；
6 阙薇,攀西地区钛砂矿成矿条件及成矿远景,矿物岩石地球化学通报,283-285；
7 刘英俊,勘查地球化学,北京,科学出版社,1987；
8 阙薇,攀西地区钛砂矿成矿条件及成矿远景,矿物岩石地球化学通报,283-285；
9 王中波,长江水系沉积物碎屑矿物组成及其示踪意义,沉积学报,2006(24),570-578；
10 赵红格,物源分析方法和研究进展,沉积学报,2003,21(3)：409-415；
11 吕全荣,长江口细颗粒沉积物的矿物特征和沉积分异.上海地质,1992,43(3)：18-25；
12 赵财胜,西南太平洋区域地质、成矿作用及Punda金铜矿床特征研究,长春：吉林大学,2002；
13 卫敏,印度尼西亚桑义赫岛海滨砂矿可选性试验研究,矿产保护与利用,2009(2),33-36；
14 裴荣富,特大型矿床研究若干问题探讨,中国地质,2001(7),9-15；
15 朱章显,苏拉威西埃达克岩、类埃达克岩分布与特征,吉林大学学报,2009(39)；
16 丁清峰,东南亚北加里曼丹新生代碰撞造山带演化与成矿[J].吉林大学学报：地球科学版,2004,34(2),193-200；
17 周蒂,南沙海区及邻区构造演化动力学的若干问题[J].大地构造与成矿学,2005,29(3)：339-345；
18 郭依辉,南沙海域东南部地形地貌特征,南沙海域东南部地质地球物理综合研究专辑,武汉,中国地质大学出版社,1996,26-39；
19 吕新彪,长江中下游地区地质异常与成矿,地质学报,1998,72(3)：260-266；
20 薛君治,成因矿物学,武汉：地质出版社,1986.23-35；
21 孙玉波.1982,重力选矿.北京：冶金工业出版社；
22 高树学,2006,黑龙江省桦南砂金矿区砂金成矿物质来源及成因,采矿技术,Vol.6 No.3,591-593;
23 虞平,2007,近两年我国锆英砂及其精矿进口情况分析,市场分析与预测,Vol.26,No.8,20-24：
24 吕英杰,1988,辽宁、吉林、黑龙江地区流水成因的砂金矿,中国地质科学院院报,(18)70-90;
25 唐鑫,从板块构造观点论南海的成因1地球物理学报,1981,24(4)
26 万平益,巴山锰矿带地质特征、矿床成因及成矿远景分析,中国锰业,四川省冶金地质勘查局六O四大队；
27 阙薇,2008,攀枝花市钛砂矿成矿远景预测,No1,61-62；
28 方念乔,印度尼西亚多岛海沉积记录基本特征与云南古特提斯研究,地学前缘,2002,Vol9,No.3,79-87；
29 D.E考克斯、D.A.辛格,1986(宋伯庆等,1990译),矿床模式,地质出版社,33-44；
30 王昆山,长江水下三角洲沉积物的重矿物分布及组合,海洋地质与第四纪地质,2007(27)7-12
31 丁清峰,东南亚北加里曼丹新生代碰撞造山带演化与成矿,2004(34)：193-200；
32 王昆山,长江水下三角洲沉积物的重矿物分布及组合,海洋地质与第四纪地质,2007(27),8-12;
33 林晓彤等黄河物源碎屑沉积物的重矿物特征,海洋地质与第四纪地质,2003,23(3)：17-21；
34地矿部海洋地质研究所,中国的海洋砂矿,中国地质,1998(4)23-26；
35 王正铤,中国滨海砂矿成矿带,中国地质科学院天津地质扩产研究所所刊,1988(20)114-126：
36 杨森楠,中、新生代太平洋陆缘带的构造格局和构造转换,地学前缘(中国地质大学,北京),1997(4)247-255；
37 张宝柱,印度尼西亚地质矿产考察报告云南地质科技情报论文,云南地质科技情报,62-74；
38 王鸿祯,中国东部及邻区中、新生代盆地发育及大陆边缘区的构造发展,地质学报,1983,57(2)：213-223
39 殷鸿福等,中国古生物地理学1武汉：中国地质大学出版社,1988；
40 涂怀奎,冲积型金刚石砂矿与其成矿模式的讨论,化工矿产地质,2001(23)239-244；
41 沈若慧,台湾海峡西部海底有用重砂高品位分布与找矿意义,台湾海峡,1999(18),131-138：
42 李旭,加里曼丹及邻区壳体的运动与演化,大地构造与成矿学,2002(9)235-239；
43 Morton A and Hurst A. Correlation of sandstones using heavy minerals:an examp le from the Statfjord Formation of the Snorre Field, northern North Sea. In:Dunay R E, Hailwood E A, eds. Nonbiostrati-graphicalMethods of Dating and Correlation. Geological Society Special Publication,1995,89:3-22.
44 Duan Chenglong. An Analysis and Evaluation for the Situation of Titanium Resources. Sichuan Nonferrous metals,2000(2):31-34;
45 Pakiser L C, Zietz I. Transcontinental crust and upper mantle structure. Revs Geophys, 1965, (3):505-520;
46 Livaccari R F. Role of crustal thickening and extensional collapse in the tectonic evolution of the Sevier-Laramide orogeny western United States. Geol,1991,19(11): 1104-1107;
47 Jones D L, Cox A, Coney P, Beck M. The growth of western North America.Scientific American,1982,247(5):70-84;
48 Runcorn S K. Satellite gravity measurements and liminar viscous flow model of the Earth's mantle, J Geophys Res,1976(14):375-384;
49 Kaula W M. Global gravity and mantle convection. Tectonophysics,1972,13:341-359;
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51 Howells C. Tertiary response to oblique subduction and indentation in Sumatra, Indonesia:New ideas for hydrocarbon exploration. Petroleum Geology of Southeast Asia:Geological society special publication,1997,126:365-374;
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