粤北大沟谷热水沉积钠长石岩岩石化学及稀土元素

梁华英; 王秀璋; 程景平

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

粤北大沟谷热水沉积钠长石岩岩石化学及稀土元素

梁华英, 王秀璋, 程景平

文章导航 > 沉积学报 > 2001 > 19(3): 415-420

梁华英, 王秀璋, 程景平. 粤北大沟谷热水沉积钠长石岩岩石化学及稀土元素[J]. 沉积学报, 2001, 19(3): 415-420.

引用本文:

梁华英, 王秀璋, 程景平. 粤北大沟谷热水沉积钠长石岩岩石化学及稀土元素[J]. 沉积学报, 2001, 19(3): 415-420.

LIANG Hua ying, WANG Xiu zhang, CHENG Jing ping. Chemical Composition and REE Pattern of Hydrothermally Deposited Albitite in Northern Guangdong Province[J]. Acta Sedimentologica Sinica, 2001, 19(3): 415-420.

Citation:

LIANG Hua ying, WANG Xiu zhang, CHENG Jing ping. Chemical Composition and REE Pattern of Hydrothermally Deposited Albitite in Northern Guangdong Province[J]. Acta Sedimentologica Sinica, 2001, 19(3): 415-420.

梁华英, 王秀璋, 程景平. 粤北大沟谷热水沉积钠长石岩岩石化学及稀土元素[J]. 沉积学报, 2001, 19(3): 415-420.

引用本文:

梁华英, 王秀璋, 程景平. 粤北大沟谷热水沉积钠长石岩岩石化学及稀土元素[J]. 沉积学报, 2001, 19(3): 415-420.

Citation:

粤北大沟谷热水沉积钠长石岩岩石化学及稀土元素

中国科学院广州地球化学研究所,广州 510640

基金项目: 国家自然科学基金(批准号:49772114);中国科学院重点项目KZ952-91-435资助项目

详细信息

中图分类号: P595

计量

文章访问数: 636
HTML全文浏览量: 4
PDF下载量: 326
被引次数: 0

Chemical Composition and REE Pattern of Hydrothermally Deposited Albitite in Northern Guangdong Province

Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640

摘要

摘要: 大沟谷含金钠长石岩带上为层状下为脉状产于震旦系乐昌峡群片岩中,主要由钠长石岩及碳酸盐岩组成。钠长石岩多为块状及条带状构造。钠长石岩和片岩化学成分不同,钠长石岩相对富集Al₂ O₃ 、TiO₂ 、MnO、Na₂O、P₂O₅,而贫Fe₂O₃ 、FeO、MgO、CaO、K₂ O。在主要氧化物组成的直角坐标图上,钠长石岩和片岩位于不同的区域及具不同的变化趋势。钠长石岩稀土元素含量较低,在 12.5 6× 10 ^-6～ 5 5.6 6× 10 ^-6之间,具较低的La/Yb(1.82～ 6.42 )、La/Sm(0.96～ 2.99)、Gd/Yb(0.99～ 2.71)比值,较大的δEu异常范围 (0.41～ 0.8),弱的δCe异常。钠长石岩地质产状特征及稀土元素特征表明其主要是热水沉积形成的。
- 钠长石岩 /
- 稀土元素 /
- 热水沉积 /
- 粤北
Abstract: Dagougu gola-bearing albitite belt,composed of albitite and carbonate rock,occurred as stratiform in the upper part and filled veins in the lower part in the Lechangxia Group Schist,Sinian Period．The albitite usually with banded and massive structure is composed primary of albite(80％±),quartz(1％～15％±),carbonate rock(1％--5％±),rutile(1％±),apatite(1％±)and pyrite with minor tourmnaline and magnetite；the carbonate rock。occurred in the same occurrence as those of albitite,consists predominantly of dolomite(ankerite)(> 75％),calcite(>15％),albite(5％±)with the same minor minerals as those of albitite． Main element compositions of the albitite differ from that of the Lechangxia Group Schist,the former is rich in A1₂O₃。TiO₂,Mno,Na₂O。P₂O₅ and poor in Fe₂O₃,Feo,Mgo,Cao,K₂O．The albitite and adjacent I．Lechangxia Group Schist lie in different domains in the major oxides variation diagram including TiO₂-A1₂O₃, AL₂O₃一SiO₂,Mgo-Sio,TiO₂-SiO₂,Feo-Fe₂O₃,Mgo-Cao and reveal different variation tendency． The albitite has lower REE content,raring from l2．56×10^-6to 55．66*10^-6with lower La/Yb：1．82～6．42,La/Sm：0．96～2．99,Gd/Yb：O．99-2．71 ratios,negative Eu anomalies and weakly Ce anomalies．Chondrite-normalized patterns of REE in albitite differ from those of the Lechangxia Group Schist． Ccmbined field and geochemical data indicate that the Dagougu gold-bearing stratiform albitite do not represent the normal clastic sedimeents altered by sodium rich fluid．but owe its origin to hydrothermal sedimentation at or below the sediment-wlater interface in alkaline environment．
- albitite /
- REE /
- hydrothermal sedimentation Northern /
- Guangdong

HTML全文

参考文献(1)

[1]

1.Rona P A H-ydrothermal mineralization deposits in ocean crust 1978(02)

2.陈先沛;高计元;陈多福热水沉积作用的概念和几个岩石学标志 1992(03)

3.祁思敬;李英;曾章仁秦岭热水沉符号型铅锌(铜)矿床 1993

4.祁思敬;李英秦岭泥盆系铅锌成矿带 1993

5.韩发;R W哈钦林大厂锡多金属矿床热液喷气沉积的证据-含矿建造及热液沉积岩[期刊论文]-矿床地质 1989(02)

6.韩发;孙海田Sedex型矿床成矿系统[期刊论文]-地学前缘 1999(01)

7.Lijima A;HeinJR Siliceous deposits in Pacific region,Develop-ments in sedimentology 36 1983

8.Herzing P M Hydrothermal silica chimner field in Galapayos spreeding center at 86w 1988(01)

9.AdachiM;Yamamoto K;Suigisk R Hydrothermal chert and associat-ed siliceous rocks from the Northem Pacific:their geological significance as indication of ocean ridge a ctiving 1986(1-2)

10.周永章丹池盆地热水沉成因硅质岩地球化学特征 1990(03)

11.Bostroem K Genesis of ferromanganese deposits-diagnostic criteria from recent and old deposits1983

12.Fle Hydrothermal and hydrogeneous ferromanganes deposits 1983

13.Slack J F;Herriman N;Bames R Stratiform toumalinites in metamorphic teranes and their geological significance 1984(12)

14.Plimer IR Tourmalinites associated with Australia proterozoic subma-rine exhalative ores 1988

15.Taylor B E;Slack J F Tourraline from Appalachian-Caledonian mas-sive sulfide deposits: textural,chemical and isotopic relationships 1984

16.Willner A P Torumalinites from the stratiform peraluminous mmta-morphic suit of the Central Namaqua Mobile Belt (South Africa) 1992

17.张奋生;彭少梅;伍广宇粤北新州地区乐昌峡群的层序和特征 1991(03)

18.彭少梅粤北大沟谷碎裂钠长石岩型金矿床的构造-热液成矿机理 1993

19.Slack J F Origin and significance of Tourmaline-rich rocks in the Bro-ken HiAll destrict,Australia 1993(03)

20.Qi Lia ng;HuJing;Gregoire D C Determination of trace elements ingranites by inductively coupledplasma mass spectrometry[外文期刊] 2000

21.朱大岗粤北大沟谷式金矿床地质特征及成因探讨 1994(03)

22.王中刚;于学元;赵振华稀土元素地球化学 1989

23.季克俭热液矿床的矿源水源及热源以及矿床分布规律 1992

24.Klinkhammer G Rare earth elements in seawater near hy-drothermal vents 1983

25.Marchard A Rareearthelementsanduraniuminhigh-tempera-ture solutions from East pacific Rise hydrothermal vent field (13N) 1983

26.Eugster H P;Jones B F Gels composed of sodium-aluminum silicate,Lake Magadi, Kenya 1968

27.Coveney R M;Kelly W C Dawsonite as a daughter mineral in hy-drothermal fluid inclusions 1971(04)

[1]	宋世骏, 柳益群, 郑庆华, 周鼎武, 付瑜. 鄂尔多斯盆地三叠系延长组黑色岩系成因探讨——以铜川地区长7₃段为例 . 沉积学报, 2019, 37(6): 1117-1128. doi: 10.14027/j.issn.1000-0550.2019.053
[2]	. 辽东湾东南部海域柱状沉积物稀土元素地球化学特征与物源识别 . 沉积学报, 2014, 32(4): 684-691.
[3]	陈文彬. 羌塘盆地那底岗日地区布曲组碳酸盐岩烃源岩稀土元素分布特征及意义 . 沉积学报, 2011, 29(3): 529-536.
[4]	龚玲兰. 湘江悬浮物的稀土元素地球化学研究 . 沉积学报, 2009, 27(3): 529-536.
[5]	刘长江. 淄博煤田煤的稀土元素地球化学特征 . 沉积学报, 2008, 26(6): 1027-1034.
[6]	刘建清. 羌塘盆地中央隆起带南侧隆额尼—昂达尔错布曲组古油藏白云岩稀土元素特征及成因意义 . 沉积学报, 2008, 26(1): 28-38.
[7]	伊海生. 西藏高原沱沱河盆地渐新世—中新世湖相碳酸盐岩稀土元素地球化学特征与正铕异常成因初探 . 沉积学报, 2008, 26(1): 1-10.
[8]	李军. 渤海湾盆地石炭二叠系稀土元素特征及其地质意义 . 沉积学报, 2007, 25(4): 589-596.
[9]	陈翠华, 何彬彬, 顾雪祥, 刘建明. 桂西北高龙金矿床含矿硅质岩成因及沉积环境分析 . 沉积学报, 2004, 22(1): 54-58.
[10]	于炳松, 陈建强, 李兴武, 林畅松. 塔里木盆地肖尔布拉克剖面下寒武统底部硅质岩微量元素和稀土元素地球化学及其沉积背景 . 沉积学报, 2004, 22(1): 59-66.
[11]	温汉捷, 裘愉卓, 凌宏文, 于柄松, 张贵山. 中国早古生代若干高硒黑色岩系中层状硅质岩的地球化学特征及其成因意义 . 沉积学报, 2003, 21(4): 620-626.
[12]	宋天锐, 和政军, 万渝生, 张巧大, 丁孝忠. 前寒武纪沉积岩中自生独居石的发现及其意义 . 沉积学报, 2003, 21(1): 118-124.
[13]	解启来, 陈多福, 漆亮, 陈先沛. 贵州瓮安陡山沱组磷块岩稀土元素地球化学特征与沉积期后变化 . 沉积学报, 2003, 21(4): 627-633.
[14]	赵志根, 唐修义, 李宝芳. 淮南矿区煤的稀土元素地球化学 . 沉积学报, 2000, 18(3): 453-459.
[15]	宋天锐. 大连地区前寒武纪沉积岩中发现自生独居石及其意义 . 沉积学报, 1999, 17(S1): 663-667.
[16]	余素华, 郑洪汉. 宁夏中卫长流水剖面沉积物中稀土元素及其环境意义 . 沉积学报, 1999, 17(1): 149-155.
[17]	陈多福, 陈光谦, 陈先沛, 高计元, 潘晶铭. 广东热水沉积超大型矿床的控矿岩石组合-礁硅岩套及其形成作用探讨 . 沉积学报, 1997, 15(S1): 91-95.
[18]	宋春晖, 武安斌, 周少平. 西成矿田海底热水喷溢沉积成因硅质岩及其与矿化关系 . 沉积学报, 1992, 10(4): 60-67.
[19]	赵一阳, 王金土, 秦朝阳, 陈毓蔚, 王贤觉, 吴明清. 中国大陆架海底沉积物中的稀土元素 . 沉积学报, 1990, 8(1): 35-43.
[20]	周永章. 丹池盆地热水成因硅岩的沉积地球化学特征 . 沉积学报, 1990, 8(3): 75-83.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 636
HTML全文浏览量: 4
PDF下载量: 326
被引次数: 0

粤北大沟谷热水沉积钠长石岩岩石化学及稀土元素

中国科学院广州地球化学研究所,广州 510640

基金项目: 国家自然科学基金(批准号:49772114);中国科学院重点项目KZ952-91-435资助项目

收稿日期: 2000-05-24
修回日期: 2000-08-01
刊出日期: 2001-09-10

中图分类号: P595

关键词:

摘要: 大沟谷含金钠长石岩带上为层状下为脉状产于震旦系乐昌峡群片岩中,主要由钠长石岩及碳酸盐岩组成。钠长石岩多为块状及条带状构造。钠长石岩和片岩化学成分不同,钠长石岩相对富集Al₂ O₃ 、TiO₂ 、MnO、Na₂O、P₂O₅,而贫Fe₂O₃ 、FeO、MgO、CaO、K₂ O。在主要氧化物组成的直角坐标图上,钠长石岩和片岩位于不同的区域及具不同的变化趋势。钠长石岩稀土元素含量较低,在 12.5 6× 10 ^-6～ 5 5.6 6× 10 ^-6之间,具较低的La/Yb(1.82～ 6.42 )、La/Sm(0.96～ 2.99)、Gd/Yb(0.99～ 2.71)比值,较大的δEu异常范围 (0.41～ 0.8),弱的δCe异常。钠长石岩地质产状特征及稀土元素特征表明其主要是热水沉积形成的。

English Abstract

Chemical Composition and REE Pattern of Hydrothermally Deposited Albitite in Northern Guangdong Province

Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640

Received Date: 2000-05-24
Rev Recd Date: 2000-08-01
Publish Date: 2001-09-10

Keywords:

Abstract: Dagougu gola-bearing albitite belt,composed of albitite and carbonate rock,occurred as stratiform in the upper part and filled veins in the lower part in the Lechangxia Group Schist,Sinian Period．The albitite usually with banded and massive structure is composed primary of albite(80％±),quartz(1％～15％±),carbonate rock(1％--5％±),rutile(1％±),apatite(1％±)and pyrite with minor tourmnaline and magnetite；the carbonate rock。occurred in the same occurrence as those of albitite,consists predominantly of dolomite(ankerite)(> 75％),calcite(>15％),albite(5％±)with the same minor minerals as those of albitite． Main element compositions of the albitite differ from that of the Lechangxia Group Schist,the former is rich in A1₂O₃。TiO₂,Mno,Na₂O。P₂O₅ and poor in Fe₂O₃,Feo,Mgo,Cao,K₂O．The albitite and adjacent I．Lechangxia Group Schist lie in different domains in the major oxides variation diagram including TiO₂-A1₂O₃, AL₂O₃一SiO₂,Mgo-Sio,TiO₂-SiO₂,Feo-Fe₂O₃,Mgo-Cao and reveal different variation tendency． The albitite has lower REE content,raring from l2．56×10^-6to 55．66*10^-6with lower La/Yb：1．82～6．42,La/Sm：0．96～2．99,Gd/Yb：O．99-2．71 ratios,negative Eu anomalies and weakly Ce anomalies．Chondrite-normalized patterns of REE in albitite differ from those of the Lechangxia Group Schist． Ccmbined field and geochemical data indicate that the Dagougu gold-bearing stratiform albitite do not represent the normal clastic sedimeents altered by sodium rich fluid．but owe its origin to hydrothermal sedimentation at or below the sediment-wlater interface in alkaline environment．