GEOCHEMISTRY AND FORMATION ENVIRONMENT OF THE LATE TRIASSIC-MIDDLE JURASSIC SILICEOUS ROCKS IN EASTERN HEILONGJIANG PROVINCE

SUN Lei; ZENG Zhen; CUI Wei-long; WANG Xiao-jie; ZHAO Qing-nian; HAO Zhen-qun; LI Han; ZHANG Hong-ze; ZHOU Jiang

doi:10.13686/j.cnki.dzyzy.2021.06.001

2021 Vol. 30, No. 6

Article Contents

Article navigation > Geology and Resources > 2021 > 30(6): 637-645

Next Article Previous Article

SUN Lei, ZENG Zhen, CUI Wei-long, WANG Xiao-jie, ZHAO Qing-nian, HAO Zhen-qun, LI Han, ZHANG Hong-ze, ZHOU Jiang. GEOCHEMISTRY AND FORMATION ENVIRONMENT OF THE LATE TRIASSIC-MIDDLE JURASSIC SILICEOUS ROCKS IN EASTERN HEILONGJIANG PROVINCE[J]. Geology and Resources, 2021, 30(6): 637-645. doi: 10.13686/j.cnki.dzyzy.2021.06.001

Citation:

SUN Lei, ZENG Zhen, CUI Wei-long, WANG Xiao-jie, ZHAO Qing-nian, HAO Zhen-qun, LI Han, ZHANG Hong-ze, ZHOU Jiang. GEOCHEMISTRY AND FORMATION ENVIRONMENT OF THE LATE TRIASSIC-MIDDLE JURASSIC SILICEOUS ROCKS IN EASTERN HEILONGJIANG PROVINCE[J]. Geology and Resources, 2021, 30(6): 637-645. doi: 10.13686/j.cnki.dzyzy.2021.06.001

GEOCHEMISTRY AND FORMATION ENVIRONMENT OF THE LATE TRIASSIC-MIDDLE JURASSIC SILICEOUS ROCKS IN EASTERN HEILONGJIANG PROVINCE

1.
Shenyang Center of China Geological Survey, Shenyang 110034, China
2.
China Aerospace Architecture Design and Research Institute Co., Ltd., Beijing 100162, China
3.
College of Earth Sciences, Jilin University, Changchun 130061, China
4.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

More Information

Corresponding author: ZENG Zhen, 23911989@qq.com

Received Date: 08 May 2019

Revised Date: 13 April 2021

Publish Date: 28 December 2021

Abstract

Abstract

The Nadanhada accretionary complex in eastern Heilongjiang Province is mainly composed of the Late Triassic-Middle Jurassic radiolarian siliceous rocks intercalated with the mafic-ultramafic complex and Late Paleozoic shallow sea sedimentary rocks. The analysis results of siliceous rocks from Shichang, Qindeli and Shengli Farm areas in eastern Heilongjiang Province show that the samples, characterized by generally low Al₂O₃, TiO₂, CaO and ΣREE contents and low Al₂O₃/(Al₂O₃+TFe₂O₃) ratio and high SiO₂ content, are pure siliceous rocks. Combined with the Al-Fe-Mn triangle diagram and K₂O/Na₂O ratio, it is indicated that the formation of siliceous rocks has nothing to do with seafloor hydrothermal process. The element discrimination diagram and geochemical characteristics reveal the siliceous rocks in the above three areas were formed in continental slope and marginal sea environment.
- siliceous rock /
- Late Triassic-Middle Jurassic /
- geochemical characteristic /
- formation environment /
- Heilongjiang Province

FullText(HTML)

References

[1]	吴福元, 曹林. 东北亚地区的若干重要基础地质问题[J]. 世界地质, 1999, 18(2): 1-13. Google Scholar Wu F Y, Cao L. Some important problems of geology in northeastern Asia[J]. World Geology, 1999, 18(2): 1-13. Google Scholar
[2]	吴福元, Wilde S, 孙德有. 佳木斯地块片麻状花岗岩的锆石离子探针U-Pb年龄[J]. 岩石学报, 2001, 17(3): 443-452. Google Scholar Wu F Y, Wilde S, Sun D Y. Zircon SHRIMP U-Pb ages of gneissic granites in Jiamusi massif, northeastern China[J]. Acta Petrologica Sinica, 2001, 17(3): 443-452. Google Scholar
[3]	Wilde S A, Zhang X Z, Wu F Y. Extension of a newly identified 500 Ma metamorphic terrane in North East China: Further U-Pb SHRIMP dating of the Mashan complex, Heilongjiang Province, China[J]. Tectonophysics, 2000, 328(1/2): 115-130. Google Scholar
[4]	Wilde S A, Wu F Y, Zhang X Z. Late Pan-African magmatism in northeastern China: SHRIMP U-Pb zircon evidence from granitoids in the Jiamusi massif[J]. Precambrian Research, 2003, 122(1/4): 311-327. Google Scholar
[5]	Sengor A M C, Natal'in B A. Paleotectonics of Asia: Fragments of a synthesis[M]//Yin A, Harrison M. The tectonic evolution of Asia. Cambridge: Cambridge University Press, 1996: 486-640. Google Scholar
[6]	Li J Y. Permian geodynamic setting of Northeast China and adjacent regions: Closure of the Paleo-Asian Ocean and subduction of the Paleo-Pacific Plate[J]. Journal of Asian Earth Sciences, 2006, 26(3/4): 207-224. Google Scholar
[7]	张贻侠, 孙运生, 张兴洲, 等. 中国满洲里-绥芬河地学断面[M]. 北京: 地质出版社, 1998: 1-34. Google Scholar Zhang Y X, Sun Y S, Zhang X Z, et al. The Manzhouli-Suifenhe geoscience section, China[M]. Beijing: Geological Publishing House, 1998: 1-34. (in Chinese) Google Scholar
[8]	Zhang X Z, Guo Y, Zhou J B, et al. Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern Northeastern China[J]. Russian Journal of Pacific Geology, 2015, 9(1): 1-10. doi: 10.1134/S181971401501008X CrossRef Google Scholar
[9]	王成文, 金巍, 张兴洲, 等. 东北及邻区晚古生代大地构造属性新认识[J]. 地层学杂志, 2008, 32(2): 119-136. doi: 10.3969/j.issn.0253-4959.2008.02.001 CrossRef Google Scholar Wang C W, Jin W, Zhang X Z, et al. New understanding of the Late Paleozoic tectonics in Northeastern China and adjacent areas[J]. Journal of Stratigraphy, 2008, 32(2): 119-136. doi: 10.3969/j.issn.0253-4959.2008.02.001 CrossRef Google Scholar
[10]	Khanchuk A I. Pre-Neogene tectonics of the Sea-of-Japan region: a view from the Russian side[J]. Earth Science, 2001, 55(5): 275-291. Google Scholar
[11]	Sengor A M C, Natal'in B A, Burtman V S. Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia[J]. Nature, 1993, 364(6435): 299-307. doi: 10.1038/364299a0 CrossRef Google Scholar
[12]	Xiao W J, Windley B F, Hao J, et al. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: Termination of the central Asian orogenic belt[J]. Tectonics, 2003, 22(6): 1069. Google Scholar
[13]	Windley B F, Alexeiev D, Xiao W J, et al. Tectonic models for accretion of the Central Asian orogenic belt[J]. Journal of the Geological Society, 2007, 164(1): 31-47. doi: 10.1144/0016-76492006-022 CrossRef Google Scholar
[14]	Faure M, Natal'in B. The geodynamic evolution of the eastern Eurasian margin in Mesozoic times[J]. Tectonophysics, 1992, 208(4): 397-411. doi: 10.1016/0040-1951(92)90437-B CrossRef Google Scholar
[15]	Natal'in B. History and modes of Mesozoic accretion in southeastern Russia[J]. Island Arc, 1993, 2(1): 15-34. doi: 10.1111/j.1440-1738.1993.tb00072.x CrossRef Google Scholar
[16]	曾振, 张兴洲, 周建波, 等. 跃进山杂岩中二叠纪变玄武岩的锆石U-Pb年代学、地球化学及其地质意义[J]. 大地构造与成矿学, 2018, 42(2): 365-378. Google Scholar Zeng Z, Zhang X Z, Zhou J B, et al. Geochemistry and zircon U-Pb age of Permian metabasalts in the Yuejinshan complexes and its tectonic implications[J]. Geotectonica et Metallogenia, 2018, 42(2): 365-378. Google Scholar
[17]	崔维龙. 佳木斯地块东缘二叠纪俯冲洋壳的发现及意义[D]. 长春: 吉林大学, 2018. Google Scholar Cui W L. The discovery and significance of Permian subducting oceanic crust on the eastern margin of Jiamusi massif, NE China[D]. Changchun: Jilin University, 2018. Google Scholar
[18]	张庆龙, 水谷伸治郎, 小智, 等. 黑龙江省那丹哈达地体构造初探[J]. 地质论评, 1989, 35(1): 67-71. doi: 10.3321/j.issn:0371-5736.1989.01.008 CrossRef Google Scholar Zhang Q L, Shinjino M, Satoru K, et al. The Nadanhada terrane in Heilongjiang Province[J]. Geological Review, 1989, 35(1): 67-71. doi: 10.3321/j.issn:0371-5736.1989.01.008 CrossRef Google Scholar
[19]	黑龙江省地质矿产局. 黑龙江省区域地质志[M]. 北京: 地质出版社, 1993: 1-619. Google Scholar Bureau of Geology and Mineral Resources of Heilongjiang Province. Regional geology of Heilongjiang Province[M]. Beijing: Geological Publishing House, 1993: 1-619. (in Chinese) Google Scholar
[20]	Kojima S. Mesozoic terrane accretion in Northeast China, Sikhote-Alin and Japan regions[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1989, 69: 213-232. doi: 10.1016/0031-0182(89)90165-X CrossRef Google Scholar
[21]	Mizutani S, Kojima S. Mesozoic radiolarian biostratigraphy of Japan and collage tectonics along the eastern continental margin of Asia[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1992, 96(1/2): 3-22. Google Scholar
[22]	张庆龙, 水谷伸治郎, 小智. 放射虫化石及地体对比研究[J]. 古生物学报, 1997, 36(2): 245-252. Google Scholar Zhang Q L, Shinjino M, Satoru K. Radiolaria and correlation study of terranes[J]. Acta Palaeontologica Sinica, 1997, 36(2): 245-252. Google Scholar
[23]	布锐G I. 东北那达哈达岭硅质岩中的三叠纪牙形刺[J]. 微体古生物学报, 1996, 13(2): 207-214. Google Scholar Buryi G I. Triassic conodonts from the cherts of Nadanhada range, northeast China[J]. Acta Micropalaeontologica Sinica, 1996, 13(2): 207-214. Google Scholar
[24]	李朋武, 张世红, 申宁华. 黑龙江省那丹哈达与日本美浓地区古地磁结果对比及意义[J]. 长春地质学院学报, 1997, 27(1): 62-66. Google Scholar Li P W, Zhang S H, Shen N H. The contrast of paleomagnetic results between Nadanhada area, Heilongjiang province and Mino area, Japan, and its significance[J]. Journal of Changchun University of Earth Sciences, 1997, 27(1): 62-66. Google Scholar
[25]	马金萍, 张婷婷, 薛林福. 黑龙江东部晚三叠世-早侏罗世放射虫硅质岩特征及油气远景[J]. 地质与资源, 2008, 17(4): 312-313, 317. doi: 10.3969/j.issn.1671-1947.2008.04.015 CrossRef Google Scholar Ma J P, Zhang T T, Xue L F. Characteristics of the T₃-J₁ radiolarian chert and potential for hydrocarbon in eastern Heilongjiang Province[J]. Geology and Resources, 2008, 17(4): 312-313, 317. doi: 10.3969/j.issn.1671-1947.2008.04.015 CrossRef Google Scholar
[26]	水谷伸治郎, 邵济安, 张庆龙. 那丹哈达地体与东亚大陆边缘中生代构造的关系[J]. 地质学报, 1989(3): 204-216. doi: 10.3321/j.issn:0001-5717.1989.03.005 CrossRef Google Scholar Shinjino M, Shao J A, Zhang Q L. The Nadanhada terrane in relation to Mesozoic tectonics on continental margins of east Asia[J]. Acta Geological Sinica, 1989(3): 204-216. doi: 10.3321/j.issn:0001-5717.1989.03.005 CrossRef Google Scholar
[27]	杨惠心, 李朋武, 禹惠民. 中国东北地区主要地体古地磁学研究[J]. 长春科技大学学报, 1998, 28(2): 203-205, 212. Google Scholar Yang H X, Li P W, Yu H M. Palaeomagnetic study of the main terranes, northeast area, China[J]. Journal of Changchun University of Science and Technology, 1998, 28(2): 203-205, 212. Google Scholar
[28]	邵济安, 王成源, 唐克东, 等. 那丹哈达岭地层与地体的关系[J]. 地层学杂志, 1990, 14(4): 286-291. Google Scholar Shao J A, Wang C Y, Tang K D, et al. Relationship between strata and terrane of the Nadanhada range[J]. Journal of Stratigraphy, 1990, 14(4): 286-291. Google Scholar
[29]	张世红, 施央申, 孙岩, 等. 黑龙江完达山造山带及其与那丹哈达地体的关系[J]. 南京大学学报(地球科学), 1991, 3(3): 287-294. Google Scholar Zhang S H, Shi Y S, Sun Y, et al. On the relation between Wandashan orogenic belt and Nadanhada terrane in Heilongjiang province[J]. Journal of Nanjing University (Earth Sciences), 1991, 3(3): 287-294. Google Scholar
[30]	曾允孚, 夏文杰. 沉积岩石学[M]. 北京: 地质出版社, 1986: 190-199. Google Scholar Zeng Y F, Xia W J. Sedimentary petrology[M]. Beijing: Geological Publishing House, 1986: 190-199. Google Scholar
[31]	Murray R W, Brink M R B T, Gerlach D C, et al. Rare earth, major, and trace element composition of Monterey and DSDP chert and associated host sediment: Assessing the influence of chemical fractionation during diagenesis[J]. Geochimica et Cosmochimica Acta, 1992, 56(7): 2657-2671. doi: 10.1016/0016-7037(92)90351-I CrossRef Google Scholar
[32]	Haskin L A, Haskin M A, Frey F A, et al. Relative and absolute terrestrial abundances of the rare earths[M]//Ahrens L H. Origin and Distribution of the Elements. Oxford: Pergamon Press, 1968: 889-912. Google Scholar
[33]	Bostrom K, Peterson M N A. The origin of aluminum-poor ferromanganoan sediments in areas of high heat flow on the East Pacific Rise[J]. Marine Geology, 1969, 7(5): 427-447. doi: 10.1016/0025-3227(69)90016-4 CrossRef Google Scholar
[34]	Girty G H, Ridge D L, Knaack C, et al. Provenance and depositional setting of Paleozoic chert and argillite, Sierra Nevada, California[J]. Journal of Sedimentary Research, 1996, 66(1): 107-118. Google Scholar
[35]	Murray R W. Chemical criteria to identify the depositional environment of chert: General principles and applications[J]. Sedimentary Geology, 1994, 90(3/4): 213-232. Google Scholar
[36]	杨建民, 王登红, 毛景文, 等. 硅质岩岩石化学研究方法及其在"镜铁山式"铁矿床中的应用[J]. 岩石矿物学杂志, 1999, 18(2): 108-120. doi: 10.3969/j.issn.1000-6524.1999.02.002 CrossRef Google Scholar Yang J M, Wang D H, Mao J W, et al. The petrochemical research method for silicalite and its application to the "Jingtieshan Type" iron deposits[J]. Acta Petrologica et Mineralogica, 1999, 18(2): 108-120. doi: 10.3969/j.issn.1000-6524.1999.02.002 CrossRef Google Scholar
[37]	Adachi M, Yamamoto K, Sugisaki R. Hydrothermal chert and associated siliceous rocks from the northern Pacific: Their geological significance as indication of ocean ridge activity[J]. Sedimentary Geology, 1986, 47(1/2): 125-148. Google Scholar
[38]	Yamamoto K. Geochemical characteristics and depositional environments of cherts and associated rocks in the Franciscan and Shimanto Terranes[J]. Sedimentary Geology, 1987, 52(1/2): 65-108. Google Scholar
[39]	张汉文. 秦岭泥盆系的热水沉积岩及其与矿产的关系——概论秦岭泥盆纪的海底热水作用[J]. 中国地质科学院西安地质矿产研究所所刊, 1991(31): 15-39. Google Scholar Zhang H W. On hydrothermal sedimentary rocks and their relationships with mineral resources in Devonian period of Qinling area, China[J]. Northwest Geoscience, 1991(31): 15-39. Google Scholar
[40]	Jones B, Manning D A C. Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones[J]. Chemical Geology, 1994, 111(1/4): 111-129. Google Scholar
[41]	Sugisaki R, Yamamoto K, Adachi M. Triassic bedded cherts in central Japan are not pelagic[J]. Nature, 1982, 298(5875): 644-647. doi: 10.1038/298644a0 CrossRef Google Scholar
[42]	杨水源, 姚静. 安徽巢湖平顶山中二叠统孤峰组硅质岩的地球化学特征及成因[J]. 高校地质学报, 2008, 14(1): 39-48. doi: 10.3969/j.issn.1006-7493.2008.01.005 CrossRef Google Scholar Yang S Y, Yao J. Geochemistry and origin of siliceous rocks from the Gufeng Formation of Middle Permian in the Pingdingshan area, Chaohu region, Anhui Province[J]. Geological Journal of China Universities, 2008, 14(1): 39-48. doi: 10.3969/j.issn.1006-7493.2008.01.005 CrossRef Google Scholar
[43]	Murray R W, Brink M R B T, Gerlach D C, et al. Rare earth, major, and trace elements in chert from the Franciscan complex and Monterey Group, California: Assessing REE sources to fine-grained marine sediment[J]. Geochimica et Cosmochimica Acta, 1991, 55(7): 1875-1895. doi: 10.1016/0016-7037(91)90030-9 CrossRef Google Scholar