GEOCHEMISTRY OF MESOZOIC GRANITOIDS IN NORTHERN DAXINGANLING MOUNTAINS: Geological Implication

LIU Xi-yao; WANG De-li; LIU Chi

2020 Vol. 29, No. 3

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LIU Xi-yao, WANG De-li, LIU Chi. GEOCHEMISTRY OF MESOZOIC GRANITOIDS IN NORTHERN DAXINGANLING MOUNTAINS: Geological Implication[J]. Geology and Resources, 2020, 29(3): 207-211, 281.

Citation:

LIU Xi-yao, WANG De-li, LIU Chi. GEOCHEMISTRY OF MESOZOIC GRANITOIDS IN NORTHERN DAXINGANLING MOUNTAINS: Geological Implication[J]. Geology and Resources, 2020, 29(3): 207-211, 281.

GEOCHEMISTRY OF MESOZOIC GRANITOIDS IN NORTHERN DAXINGANLING MOUNTAINS: Geological Implication

1.
Liaoning Institute of Geology and Mineral Survey Co., Ltd., Shenyang 110032, China
2.
Inner Mongolia No. 115 Institute of Geological and Mineral Exploration and Development, Ulanhot 137405, Inner Mongolia, China
3.
Shenyang Center of China Geological Survey, Shenyang 110034, China

Received Date: 08 January 2020

Revised Date: 18 March 2020

Publish Date: 28 June 2020

Abstract

Abstract

Based on the elemental analysis results of rock samples collected by the 1:200 000 stream sediment geochemical survey in northern Daxinganling Mountains, the paper counts the contents of 39 elements in the Mesozoic granitoids, analyzes the geochemical characteristics of elements, and presents the abundance values of elements in the Mesozoic granitoids of northern Daxinganling Mountains. It is concluded that the Mesozoic granitoids have the characteristics of potassium-rich acid granites and aluminium-rich acid-intermediate granites, which are closely related to the Mesozoic tectonic movement and magmatic activity.
- element abundance /
- geochemical characteristics /
- Mesozoic granitoid /
- Daxinganling Mountains

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References

[1]	王粉丽, 王海鹏, 鲁红峰, 等.大兴安岭北部上其地区中生代花岗岩年代学、岩石地球化学特征及构造背景[J].地质科技情报, 2016, 35(4):18-28. Google Scholar
[2]	刘俊来, Davis G A, 纪沫, 等.地壳的拆离作用与华北克拉通破坏:晚中生代伸展构造约束[J].地学前缘, 2008, 15(3):72-81. doi: 10.3321/j.issn:1005-2321.2008.03.005 CrossRef Google Scholar
[3]	吴福元, 孙德有, 林强.东北地区显生宙花岗岩的成因与地壳增生[J].岩石学报, 1999, 15(2):181-189. Google Scholar
[4]	林强, 葛文春, 吴福元, 等.大兴安岭中生代花岗岩类的地球化学[J].岩石学报, 2004, 20(3):403-412. Google Scholar
[5]	梁科伟, 李成禄, 张立东, 等.大兴安岭诺敏地区二叠纪花岗岩的地球化学特征及地质意义[J].地质与资源, 2012, 21(2):181-187. doi: 10.3969/j.issn.1671-1947.2012.02.001 CrossRef Google Scholar
[6]	刘凯, 吴涛涛, 刘金龙, 等.大兴安岭北段图里河地区满克头鄂博组火山岩年代学及地球化学[J].中国地质, 2018, 45(2):367-376. Google Scholar
[7]	胡军海, 杨华本, 周传芳, 等.大兴安岭北段漠河富源沟林场早侏罗世花岗岩——年代学、地球化学特征及构造意义[J].地质与资源, 2018, 27(3):224-234. doi: 10.3969/j.issn.1671-1947.2018.03.003 CrossRef Google Scholar
[8]	戴慧敏, 杨忠芳, 马振东, 等.大兴安岭查巴奇地区中生代侵入岩岩石地球化学特征及构造背景[J].中国地质, 2013, 40(1):232-247. doi: 10.3969/j.issn.1000-3657.2013.01.016 CrossRef Google Scholar
[9]	杜兵盈, 刘宇崴, 赵明胜, 等.大兴安岭地区加格达奇东部早白垩世火山岩地层的厘定及地质意义[J].地质与资源, 2018, 27(4):317-323. doi: 10.3969/j.issn.1671-1947.2018.04.002 CrossRef Google Scholar
[10]	乔牡冬, 孙加鹏, 李宇菡, 等.大兴安岭新林区中生代流纹岩年代学、地球化学特征及其地质意义[J].地质与资源, 2018, 27(4):324-336. doi: 10.3969/j.issn.1671-1947.2018.04.003 CrossRef Google Scholar
[11]	聂凤军, 孙振江, 刘翼飞, 等.大兴安岭岔路口矿区中生代多期岩浆活动与钼成矿作用[J].中国地质, 2013, 40(1):273-286. doi: 10.3969/j.issn.1000-3657.2013.01.018 CrossRef Google Scholar
[12]	中华人民共和国地质矿产部. DZ/T 0167-1995区域地球化学勘查规范(比例尺1: 200000)[S].北京: 地质出版社, 1996: 16-17. Google Scholar
[13]	叶家喻, 姜宝林.区域地球化学勘查样品分析方法[M].北京:地质出版社, 2004:416-417. Google Scholar
[14]	中华人民共和国国土资源部. DZ/T 0011-2015地球化学普查规范(1: 50000)[S].北京: 地质出版社, 2015: 1-34. Google Scholar
[15]	国土资源部中国地质调查局.中华人民共和国多目标区域地球化学图集-松辽平原中南部地区[M].北京:地质出版社, 2013:306-306. Google Scholar
[16]	蔡剑辉, 阎国翰, 许保良, 等.太行山-大兴安岭东麓晚中生代碱性侵入岩岩石地球化学特征及其意义[J].地球学报, 2006, 27(5):447-459. doi: 10.3321/j.issn:1006-3021.2006.05.007 CrossRef Google Scholar
[17]	程志忠, 谢学锦.岩石中元素背景值变化对地球化学成矿预测的影响[J].地质学报, 2006, 33(2):411-417. Google Scholar
[18]	史长义, 鄢明才, 迟清华.中国花岗岩类化学元素丰度[M].北京:地质出版社, 2008:1-119. Google Scholar
[19]	史长义, 鄢明才, 刘崇民, 等.中国不同岩石类型花岗岩类元素丰度及特征[J].物探化探计算技术, 2005, 27(3):256-262. doi: 10.3969/j.issn.1001-1749.2005.03.016 CrossRef Google Scholar
[20]	史长义, 鄢明才, 迟清华.中国不同构造单元花岗岩类元素丰度及特征[J].地质学报, 2007, 81(1):47-59. Google Scholar
[21]	武广, 陈衍景, 孙丰月, 等.大兴安岭北端晚侏罗世花岗岩类地球化学及其地质和找矿意义[J].岩石学报, 2008, 24(4):899-910. Google Scholar
[22]	武广, 陈衍景, 赵振华, 等.大兴安岭北端洛古河东花岗岩的地球化学、SHRIMP锆石U-Pb年龄和岩石成因[J].岩石学报, 2009, 25(2):233-247. Google Scholar
[23]	张辉, 戴朝成, 闫秋实, 等.内蒙古大桦背I型花岗岩地球化学特征及其成因意义[J].地质与资源, 2015, 24(1):12-19, 69. Google Scholar