河南嵩山地区新元古界何家寨组微亮晶(臼齿)碳酸盐岩成因新认识<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2020.01.004

古地理学报 ›› 2020, Vol. 22 ›› Issue (1): 56-74. doi: 10.7605/gdlxb.2020.01.004

• 岩相古地理学及沉积学 • 上一篇下一篇

河南嵩山地区新元古界何家寨组微亮晶(臼齿)碳酸盐岩成因新认识^*

王振涛¹, 李现根²

1 中国地质科学院矿产资源研究所自然资源部成矿作用与资源评价重点实验室,北京 100037;
2 中石化胜利油田分公司海洋采油厂,山东东营 257237

收稿日期:2018-07-29 出版日期:2020-02-01 发布日期:2020-03-04
作者简介:王振涛,男,1986年生,副研究员,2014年毕业于中国地质大学(北京)并获得博士学位,2016年中国地质科学院矿产资源研究所博士后出站,现主要从事沉积学与大地构造研究。E-mail: wangz@cags.ac.cn。本文是第一作者在著名沉积学家孟祥化教授指导下完成的本科论文部分工作的提升与延伸。
基金资助:
*国家重点研发计划课题(编号: 2017YFC0602704)和国家自然科学基金项目(编号: 40572073)联合资助

New understanding on the genetic mechanism of microsparite(molar-tooth)carbonates in the Neoproterozoic Hejiazhai Formation in Songshan area,Henan Province

Wang Zhen-Tao¹, Li Xian-Gen²

1 MNR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,CAGS,Beijing 100037,China;
2 Offshore Oil Production Plant of Sinopec Shengli Oilfield Company,Shandong Dongying 257237,China

Received:2018-07-29 Online:2020-02-01 Published:2020-03-04
About author:Wang Zhen-Tao,male,born in 1986,is an associate professor of the Institute of Mineral Resources,Chinese Academy of Geological Sciences,with a Ph.D. degree obtained from the China University of Geosciences(Beijing). He is currently engaged in Paleozoic-Mesozoic tectonics and sedimentary evolution of the western North China Craton and Yangtze Craton. E-mail: wangz@cags.ac.cn.
Supported by:
; Co-funded by the subproject of National Key R & D Program of China(No.2017YFC0602704)and the National Natural Science Foundation of China(No.40572073)

摘要/Abstract

摘要： 作为国际前寒武系碳酸盐岩研究的热点,微亮晶(臼齿)碳酸盐岩(简称MT)在前寒武纪古地理重塑、地层对比和古气候研究等方面具有重要研究意义,但对其成因机制的认识长期存在争论。华北克拉通南缘嵩山地区新元古界何家寨组发育大量MT沉积,被前人解释为地震液化的产物。文中对何家寨组MT发育层位进行了详细的形态描述、系统的微相分析和比较沉积学的研究,确定何家寨组MT沉积于碳酸盐缓坡沉积环境,发现MT具有早期成岩作用特征,其形态类型和宿主岩性、沉积环境之间存在密切关系。从多个方面对比探讨了MT微亮晶和地震“液化脉”之间的不同,明确指出,何家寨组MT的形成受到古海洋条件和沉积岩相的严格约束,具有鲜明的古环境意义,和地震没有必然的成因联系。

关键词: 嵩山地区, 何家寨组, 臼齿碳酸盐岩, 地震液化脉

Abstract: As an international research focus on the Precambrian carbonate rocks,the microsparite(molar-tooth)carbonate (MT for short)is of great significance in the reconstruction of palaeogeography,stratigraphic correlation and palaeoclimate,but its formation mechanism has been debated for a long time. The Neoproterozoic Hejiazhai Formation in Songshan area,which is located at the southern margin of North China Craton,is characterized as a large number of MT deposits that were interpreted as the product of seismic liquefaction. In this paper,based on the MT-containing strata of the Hejiazhai Formation,detailed studies include the morphology of MT,microfacies and sedimentary environment were carried out. Results show that the Hejiazhai Formation MT formed in the carbonate ramp environment and it owes early diagenetic features. The morphology of MT has a strong relationship with the lithology of the host rocks and the sedimentary environments. Besides,the differences between the MT and “liquefied vein”triggered by earthquake were compared from several aspects. Through the above work,we clearly pointed out that the Hejiazhai Formation MT is mainly constrained by the palaeomarine conditions and sedimentary microfacies,and it is a good indicator of the ancient environment,but has no relationship with the earthquakes.

Key words: Songshan area, Hejiazhai Formation, molar-tooth carbonate, seisimic liquefied vein

中图分类号:

P583

王振涛, 李现根. 河南嵩山地区新元古界何家寨组微亮晶(臼齿)碳酸盐岩成因新认识^*[J]. 古地理学报, 2020, 22(1): 56-74.

Wang Zhen-Tao, Li Xian-Gen. New understanding on the genetic mechanism of microsparite(molar-tooth)carbonates in the Neoproterozoic Hejiazhai Formation in Songshan area,Henan Province[J]. JOPC, 2020, 22(1): 56-74.

http://www.gdlxb.cn/CN/Y2020/V22/I1/56

参考文献

[1] 安徽省地质矿产局区域地质调查队. 1985. 安徽地层志(前寒武系分册). 合肥: 安徽科技出版社,1-721.
[Regional Geological Survey Team of Anhui Bureau of Geology and Mineral Resources. 1985. Stratigraphic Records of Anhui(Precambrian fascicle). Hefei: Anhui Science and Technology Press, 1-721]
[2] 第五春荣,孙勇,袁洪林,王洪亮,钟兴平,柳小明. 2008. 河南登封地区嵩山石英岩碎屑锆石 U-Pb 年代学、Hf 同位素组成及其地质意义. 科学通报, 53(16): 1923-1934.
[Diwu C R,Sun Y,Yuan H L,Wang H L,Zhong X P,Liu X M.2008. U-Pb ages and Hf isotopes for detrital zircons from quartzite in the Paleoproterozoic Songshan Group on the southwestern margin of the North China Craton. Chinese Science Bulletin,53(18): 2828-2839]
[3] 窦鲁星,冯乐,江煜波. 2014. 徐州地区新元古界贾园组臼齿构造沉积环境分析及成因探讨. 沉积与特提斯地质, 34(4): 40-47.
[Dou L X,Feng L,Jiang Y B.2014. Sedimentary environments and genesis of the molar-tooth structures in the Neoproterozoic Jiayuan Formation in the Xuzhou region,Jiangsu. Sedimentary Geology and Tethyan Geology, 34(4): 40-47]
[4] 杜远生,余文超. 2017. 地震和非地震引发的软沉积物变形. 古地理学报, 19(1): 65-72.
[Du Y S,Yu W C.2017. Earthquake-caused and non-earthquake-caused soft-sediment deformations. Journal of Palaeogeography(Chinese Edition), 19(1): 65-72]
[5] 冯乐,李壮福,陆鹿,窦鲁星,师庆民,周晏召. 2015. 徐州地区新元古界下部具臼齿构造碳酸盐岩事件成因探讨. 高校地质学报, 21(2): 203-214.
[Feng L,Li Z F,Lu L,Dou L X,Shi Q M,Zhou Y Z.2015. Study on the origin of molar-tooth structure-bearing carbonates in the lower Neoproterozoic in Xuzhou area. Geological Journal of China Universities, 21(2): 203-214]
[6] 冯增昭,鲍志东,郑秀娟,王媛. 2017. 中国软沉积物变形构造及地震岩研究简评. 古地理学报, 19(1): 7-12.
[Feng Z Z,Bao Z D,Zheng X J,Wang Y.2017. Researches of soft-sediment deformation structures and seismites in China: A brief review. Journal of Palaeogeography(Chinese Edition), 19(1): 7-12]
[7] 高林志,柳永清. 2005. 河南嵩山地区新元古界何家窑组微亮晶脉特征、成因及地质意义探讨. 地质论评, 51(4): 373-381.
[Gao L Z,Liu Y Q.2005. Microspar veins in the Neoproterozoic Hejiayao Formation in the Songshan area,Henan Province. Geological Review, 51(4): 373-381]
[8] 葛铭,孟祥化,杨遵仪. 2001. 元古代微亮晶碳酸盐岩事件和地球演化研究进展. 见: 2001年全国沉积学大会摘要论文集,266-268.
[Ge M,Meng X H,Yang Z. 2001. Recent advances on molar tooth carbonates and evolution of the Earth in the Proterozoic. In: Proceedings of the National Congress on Sedimentology in 2001, 266-268]
[9] 葛铭,孟祥化,旷红伟,蔡国印,刘燕学,刘为付. 2003. 微亮晶(臼齿)碳酸盐岩: 21世纪全球地学研究的新热点. 沉积学报, 21(1): 81-89.
[Ge M,Meng X H,Kuang H W,Cai G Y,Liu Y X,Liu W F.2003. Molar-tooth carboantes: Carbonate research highlight of the world in the 21st Century. Acta Sedimentologica Sinica, 21(1): 81-89]
[10] 葛铭,孟祥化. 2008. 古海洋中奇妙的微亮晶碳酸盐岩. 自然杂志, 30(6): 329-333.
[Ge M,Meng X H.2008. Molar-tooth Carbonates: Which is a bizarrerie rock type in paleo-ocean. Chinese Journal of Nature, 30(6): 329-333]
[11] 关保德,耿午辰,戎治权,杜慧英. 1988. 河南东秦岭北坡中—上元古界. 郑州: 河南科学技术出版社,41-49.
[Guan B D,Geng W C,Rong Z Q,Du H Y. 1988. Middle and Late Proterozoic Strata of the Northern Slope of East Qinling,Henan Province. Zhengzhou: Henan Science and Technology Press,41-49]
[12] 郭峰,孟祥化,葛铭. 2009. 安徽灵璧地区新元古代臼齿构造(微亮晶)碳酸盐沉积及意义. 安徽地质, 19(3): 176-180.
[Guo F,Meng X H,Ge M.2009. Neo-proterozoic MTS carbonatite deposition in the Lingbi area,Anhui and the implications. Geology of Anhui, 19(3): 176-180]
[13] 何镜宇,孟祥化. 1987. 沉积岩和沉积相模式及建造. 北京: 地质出版社,1-435.
[He J Y,Meng X H. 1987. Sedimentary Rocks,Sedimentary Facies Models and Formation. Beijing: Geological Publishing House,1-435]
[14] 河南省地质矿产厅. 1997. 河南省岩石地层. 武汉: 中国地质大学出版社,1-299.
[Bureau of Geology and Mineral Resources of Henan Province. 1997. Stratigraphy(Lithostratic)of Henan Province. Wuhan: China University of Geosciences Press,1-299]
[15] 胡国辉,赵太平,周艳艳,杨阳. 2012a. 华北克拉通南缘五佛山群沉积时代和物源区分析: 碎屑锆石U-Pb年龄和Hf同位素证据. 地球化学, 41(4): 326-342.
[Hu G H,Zhao T P,Zhou Y Y,Yang Y.2012a. Depositional age and provenance of the Wufoshan Group in the southern margin of the North China Craton: Evidence from detrital zircon U-Pb ages and Hf isotopic compositions. Geochimica, 41(4): 326-342]
[16] 胡国辉,周艳艳,赵太平. 2012b. 河南嵩山地区元古宙五佛山群沉积岩的地球化学特征及其对物源区和构造环境的制约. 岩石学报, 28(11): 3692-3704.
[Hu G H,Zhou Y Y,Zhao T P.2012b. Geochemistry of Proterozoic Wufoshan Group sedimentary rocks in the Songshan area,Henan Province: Implications for provenance and tectonic setting. Acta Petrologica Sinica, 28(11): 3692-3704]
[17] 胡国辉,赵太平,周艳艳,王世炎. 2013. 华北克拉通南缘中—新元古代沉积地层对比研究及其地质意义. 岩石学报, 29(7): 2491-2507.
[Hu G H,Zhao T P,Zhou Y Y,Wang S Y.2013. Meso-Neoproterozoic sedimentary formation in the southern margin of the North China Craton and its geological implications. Acta Petrologica Sinica, 29(7): 2491-2507]
[18] 嵇少丞. 2018. Seismites(地震岩)等术语的概念与名称. 中国科技术语, 20(6): 33-38.
[Ji S C.2018. On seismites,liquefactites and fault rocks. China Terminology, 20(6): 33-38]
[19] 吉林省地质矿产局. 1988. 吉林省区域地质志. 北京: 地质出版社,1-698.
[Bureau of Geology and Mineral Resources of Jilin Province. 1988. Regional Geology of Jilin Province. Beijing: Geological Publishing House, 1-698]
[20] 贾超. 2018. 豫西地区新元古代地层的形成时限、物源及构造背景分析. 合肥: 合肥工业大学,1-83.
[Jia C.2018. Depositional age,Provenance and Tectonic Background of Neoproterozoic Strata in Western Henan Province. Hefei: Hefei University of Technology,1-83]
[21] 贾志海,洪天求,郑文武,李双应. 2003. 皖北新元古代望山组震积岩的基本特征及其形成环境分析. 地层学杂志, 27(2): 146-149.
[Jia Z H,Hong T Q,Zheng W W,Li S Y.2003. The characters and environments of the Seismites of the Neoproterzoic Wangshan Formation in north Anhui. Journal of Stratigraphy, 27(2): 146-149]
[22] 贾志海. 2004. 淮南地区新元古代九里桥组沉积环境变化及其生物学响应研究. 合肥工业大学博士学位论文.
[Jia Z H.2004. A Research on the Depositional Environments Changing and Its' Biological Responsing during the Sedimentation of the Neoproterozoic Jiuliqiao Formation,Huainan Region,Anhui Province,China. Doctoral Thesis of Hefei University of Technology]
[23] 贾志海,宁霄峰,洪天求,郑文武. 2011. 苏皖北部新元古界臼齿碳酸盐岩脉类型及其形成机理. 古地理学报, 13(6): 627-634.
[Jia Z H,Ning X F,Hong T Q,Zheng W W.2011. The Neoproterozoic molar-tooth carbonate rock veins in northern Anhui and Jiangsu Provinces and their forming mechanism. Journal of Palaeogeography(Chinese Edition), 13(6): 627-634]
[24] 江苏省地质矿产局. 1984. 江苏省及上海市区域地质志. 北京: 地质出版社,1-857.
[Bureau of Geology and Mineral Resources of Jiangsu Province. 1984. Regional Geological Records of Jiangsu and Shanghai. Beijing: Geological Publishing House, 1-857]
[25] 旷红伟,金广春,刘燕学,孟祥化,葛铭. 2004a. 从地球化学角度看微亮晶臼齿碳酸盐岩形成的环境条件: 以吉辽地区新元古代微亮晶碳酸盐岩为例. 天然气地球科学, 15(2): 150-155.
[Kuang H W,Jin G C,Liu Y X,Meng X H,Ge M.2004a. the environmental conditions of the Microsparite(Molar Tooth)carbonates opened out by geochemistry: An example from the Microsparite carbonates of Neoproterozoic in Ji-Liao region,China. Natural Gas Geoscience, 15(2): 150-155]
[26] 旷红伟,金广春,刘燕学,孟祥化,葛铭. 2004b. 从地球化学角度看微亮晶臼齿碳酸盐岩形成的环境条件: 以吉辽地区新元古代微亮晶碳酸盐岩为例. 天然气地球科学, 15(2): 150-155.
[Kuang H W,Jin G C,Liu Y X,Meng X H,Ge M.2004b. the environmental conditions of the Microsparite(Molar Tooth)carbonates opened out by geochemistry: An example from the Microsparite carbonates of Neoproterozoic in Ji-Liao region,China. Natural Gas Geoscience, 15(2): 150-155]
[27] 旷红伟,刘燕学,孟祥化,葛铭,蔡国印. 2004c. 吉辽地区新元古代臼齿碳酸盐岩岩相的若干岩石学特征研究. 地球学报, 25(6): 647-652.
[Kuang H W,Liu Y X,Meng X H,Ge M,Cai G Y.2004c. Sedimentary lithofacies and petrological features of Neoproterozoic MT structures-bearing carbonates in Jilin-Liaoning area. Acta Geoscientica Sinica, 25(6): 647-652]
[28] 旷红伟,刘燕学,孟祥化,葛铭. 2005. 吉辽地区震旦系碳酸盐岩地球化学特征及其环境意义. 天然气地球科学, 16(1): 54-58.
[Kuang H W,Liu Y X,Meng X H,Ge M.2005. The geochemical features and its environmental significance of the Sinian carbonates in the Jilin-Liaoning area. Natural Gas Geoscience, 16(1): 54-58]
[29] 旷红伟,刘燕学,孟祥化,葛铭. 2006a. 吉林南部通化二道江剖面新元古界万隆组臼齿构造及其沉积特征. 古地理学报, 8(4): 457-466.
[Kuang H W,Liu Y X,Meng X H,Ge M.2006a. Molar-tooth structure and sedimentary characteristics of the Wanlong Formation of Neoproterozoic at Erdaojiang section of Tonghua County in southern Jilin Province. Journal of Palaeogeography(Chinese Edition), 8(4): 457-466]
[30] 旷红伟,孟祥化,葛铭. 2006b. 臼齿碳酸盐岩成因探讨: 以吉林—辽宁地区新元古界为例. 古地理学报, 8(1): 63-73.
[Kuang H W,Meng X H,Ge M.2006b. Discussion on origin for Molar Tooth carbonate rocks: An example from the Neoproterozoic in Jilin-Liaoning area. Journal of Palaeogeography(Chinese Edition), 8(1): 63-73]
[31] 旷红伟,金广春,刘燕学. 2008. 吉辽地区新元古代臼齿构造形态及其研究意义. 中国科学 D辑: 地球科学,38(增刊Ⅱ): 123-130.
[Kuang H W,Jin G C,Liu Y X.2009. Genesis types of the Neoproterozoic Molar tooth structures in the southeastern Jilin and eastern Liaoning Provinces and its research significances. Science in China Series D: Earth Sciences,52(Supp. Ⅰ): 135-142.
[32] 旷红伟,彭楠,罗顺社,岑超,李家华,陈铭培. 2009. 燕山中东部凌源地区雾迷山组MT构造的发现、地质特征和研究意义. 自然科学进展, 19(12): 1308-1318.
[Kuang H W,Peng N,Luo S S,Cen C,Li J H,Chen M P.2009. Discovery of MT structure and its geological features and studying significance in the eastern Yanshan in Lingyuan,Liaoning Province. Progress in Natural Science, 19(12): 1308-1318]
[33] 旷红伟,柳永清,彭楠,刘燕学,李家华. 2011a. 再论臼齿碳酸盐岩成因. 古地理学报, 13(3): 253-261.
[Kuang H W,Liu Y Q,Peng N,Liu Y X,Li J H.2011a. On origin of Molar Tooth carbonate rocks. Journal of Palaeogeography(Chinese Edition), 13(3): 253-261]
[34] 旷红伟,柳永清,彭楠,刘丽军. 2011b. 辽东大连新元古代臼齿碳酸盐岩地球化学特征及其地质意义. 地学前缘, 18(4): 25-40.
[Kuang H W,Liu Y Q,Peng N,Liu L J.2011b. Geochemistry of the Neoproterozoic molar-tooth carbonates in Dalian,eastern Liaoning,China,and its geological implications. Earth Science Frontiers, 18(4): 25-40]
[35] 旷红伟,柳永清,耿元生,白华青,彭楠,范正秀,宋换新,夏晓旭,王玉冲,陈骁帅. 2019. 中国中新元古代重要沉积地质事件及其意义. 古地理学报, 21(1): 1-30.
[Kuang H W,Liu Y Q,Geng Y S,Bai H Q,Peng N,Fan Z X,Song H X,Xia X X,Wang Y C,Chen X S.2019. Important sedimentary geological events of the Meso-Neoproterozoic and their significance. Journal of Paleogeography(Chinese Edition), 21(1): 1-30]
[36] 雷云. 2014. 球霰石型碳酸钙的研究进展. 长江大学学报(自然科学版), 11(34): 35-43.
[Lei Y.2014. Recent progress of vaterite type calcium carbonate. Journal of Yangtze University(Natural Science Edition), 11(34): 35-43]
[37] 李艳霞,旷红伟. 2012. 中国辽吉地区新元古代臼齿碳酸盐岩中分子化石及早期生命演化. 吉林大学学报(地球科学版), 42(1): 136-143.
[Li Y X,Kuang H W.2012. Molecular fossils in Neoproterozoic molar tooth carbonates from Liaoning and Jilin Provinces,China and discussion on the evolution of early life. Journal of Jilin University(Earth Science Edition), 42(1): 136-143]
[38] 辽宁省地质矿产局. 1989. 辽宁省区域地质志. 北京: 地质出版社,1-855.
[Bureau of Geology and Mineral Resources of Liaoning Province. 1989. Regional Geology of Liaoning Province. Beijing: Geological Publishing House,1-855]
[39] 刘贺娟,孟祥化,葛铭. 2012. 滇中地区大龙口组微亮晶(臼齿)碳酸盐岩研究. 岩石矿物学杂志, 31(2): 181-190.
[Liu H J,Meng X H,Ge M.2012. A study of microsparite(molar-tooth)carbonates of Dalongkou Formation in central Yunnan. Acta Petrologica Et Mineralogica, 31(2): 181-190]
[40] 刘贺娟,孙晓岭,王德海. 2013. 对前寒武纪一些沉积构造成因的思考: 以天津蓟县剖面为例. 地球科学与环境学报, 35(3): 44-54.
[Liu H J,Sun X L,Wang D H.2013. Discussion on genesis of some sedimentary structures from Precambrian: Taking Jixian section in Tianjin as an example. Journal of Earth Sciences and Environment, 35(3): 44-54]
[41] 刘礼洁,郭福生,严兆彬. 2012. 浙江桐村寒武系大陈岭组地震驱动的软沉积变形构造特征分析. 沉积学报, 30(5): 795-805.
[Liu L J,Guo F S,Yan Z B.2012. Analysis on earthquake-induced soft-sediment deformation structures in the Cambrian Dachenling Formation in the Tongcun Village,Zhejiang Province. Acta Sedimentologica Sinica, 30(5): 795-805]
[42] 刘为付,孟祥化,葛铭,刘燕学,旷红伟,蔡国印. 2003a. 皖北新元古代臼齿碳酸盐岩石学特征及沉积环境探讨. 华东地质学院学报, 26(4): 321-327.
[Liu W F,Meng X H,Ge M,Liu Y X,Kuang H W,Cai G Y.2003a. Study on petrology and sedimentary environment of molar tooth structures-bearing carbonates in Neoproterozoic in the north of Anhui. Journal of East China Geological Institute, 26(4): 321-327]
[43] 刘为付,孟祥化,葛铭,蔡国印,刘燕学,旷红伟. 2003b. 徐淮地区上元古界臼齿构造碳酸盐岩事件. 地质科技情报, 22(4): 27-32.
[Liu W F,Meng X H,Ge M,Cai G Y,Liu Y X,Kuang H W.2003b. Affairs of molar-tooth carbonates from Neoproterozoic in Xuhuai area. Geological Science and Technology Information, 22(4): 27-32]
[44] 刘为付,孟祥化,葛铭,旷红伟,刘燕学. 2004. 徐州—淮南地区新元古代臼齿碳酸盐岩成因探讨. 地质论评, 50(5): 454-463.
[Liu W F,Meng X H,Ge M,Kuang H W,Liu Y X.2004. Origin of the Neoproterozoic molar-tooth carbonates in the Xuzhou-Huaian area. Geological Review, 50(5): 454-463]
[45] 刘燕学,旷红伟,蔡国印,孟祥化,葛铭. 2003. 辽南新元古代营城子组臼齿灰岩的沉积环境. 地质通报, 22(6): 419-425.
[Liu Y X,Kuang H W,Cai G Y,Meng X H,Ge M.2003. Depositional environment of molar-tooth limestones of the Neoproterozoic Yingchengzi Formation in southern Liaoning. Geological Bulletin of China, 22(6): 419-425]
[46] 刘燕学,柳永清,旷红伟. 2005. 一种严格受控于环境和时间的特殊碳酸盐岩—臼齿构造碳酸盐岩. 地球科学进展, 20(7): 710-716.
[Liu Y X,Liu Y Q,Kuang H W.2005. Molar-tooth carbonate constrained by depositional environment and geological history. Advances in Earth Science, 20(7): 710-716]
[47] 刘自亮,孟祥化,葛铭,王德海,任国选. 2011. 蓟县高于庄组臼齿构造形态特征及成因意义. 地球学报, 32(1): 27-36.
[Liu Z L,Meng X H,Ge M,Wang D H,Ren G X.2011. Morphological characteristics and genesis of Molar-tooth structures in Gaoyuzhuang Formation of Jixian area. Acta Geoscientica Sinica, 32(1): 27-36]
[48] 柳永清,高林志,刘燕学. 2005. 苏皖辽地区新元古代微亮晶构造碳酸盐岩的沉积、岩相与环境约束. 沉积学报, 23(1): 49-59.
[Liu Y Q,Gao L Z,Liu Y X.2005. Microspar structure carbonate and constrain of sedimentary facies and environments in Jiangsu,Anhui and Liaoning Provinces of the Northern China. Acta Sedimentologica Sinica, 23(1): 49-59]
[49] 柳永清,旷红伟,彭楠,刘燕学,江小均,许欢. 2010. 中国元古代碳酸盐岩微亮晶构造及形成的沉积环境约束. 岩石学报, 26(7): 2122-2130.
[Liu Y Q,Kuang H W,Peng N,Liu Y X,Jiang X J,Xu H.2010. Proterozoic microspar and constraint of sedimentary environment in China. Acta Petrologica Sinica, 26(7): 2122-2130]
[50] 梅冥相. 2005. 天津蓟县剖面中元古界高于庄组臼齿状构造的层序地层位置及其成因的初步研究. 古地理学报, 7(4): 437-447.
[Mei M X.2005. Preliminary study on sequence-stratigraphic position and origin for Molar-tooth structure of the Gaiyuzhuang Formation of Mesoproterozoic at Jixian section in Tianjin. Journal of Palaeogeography(Chinese Edition), 7(4): 437-447]
[51] 梅冥相. 2007a. 前寒武纪“臼齿状构造迷”的一些认识: 来自天津蓟县剖面高于庄组的信息. 古地理学报, 9(6): 597-610.
[Mei M X.2007a. Some reviews on the Precambrian molar-tooth enigma: Information from the Gaoyuzhuang Formation at Jixian section in Tianjin. Journal of Palaeogeography(Chinese Edition), 9(6): 597-610]
[52] 梅冥相. 2007b. 天津蓟县中元古界高于庄组“球形臼齿状构造”新解: 1400 Ma以前球形或似球形实体宏观藻类化石的细胞显微结构. 现代地质, 21(4): 738-748.
[Mei M X.2007b. New interpretation of spheroidal molar-tooth structures from Mesoproterozoic Gaoyuzhuang Formation at the Jixian section in Tianjin: Possibly cellular microstructure of the spheroidal or the sub-spheroidal three-dimensional fossils of megascopic algae before 1400 Ma. Geoscience, 21(4): 738-748]
[53] 梅冥相. 2009. 宏观藻类化石及其相关的“前寒武纪谜”: 对天津蓟县剖面中元古代早期高于庄组第三段中一些现象的思考. 现代地质, 23(4): 616-624.
[Mei M X.2009. Brief introduction on megafossil of algae and relative Precambrian enigmas: Ponder on some phenomena from the Third Member of Gaoyuzhuang Formation of the early Mesoproterozoic at the Jixian Section. Geoscience, 23(4): 616-624]
[54] 孟祥化,葛铭,蔡国印,旷红伟,刘燕学. 2002. 下寒武统大林子组溶解蒸发岩系旋回层序及渗流构造成因. 科学通报, 47(14): 1113-1117.
[Meng X H,Ge M,Cai G Y,Kuang H W,Liu Y X.2002. Cyclic sequences of the dissolutive evaporate series and the origin of the seepage pipe structure of the Dalinzi Formation in the Lower Cambrian. Chinese Science Bulletin, 47(14): 1113-1117]
[55] 孟祥化,葛铭. 2004. 中朝板块层序·事件·演化. 北京: 科学出版社,1-548.
[Meng X H,Ge M. 2004. Cyclic Sequences,Events and the Evolution of the Sino-Korean Plate. Beijing: Science Press,1-548]
[56] 孟祥化,葛铭,旷红伟,Nielsen J K.2006. 微亮晶(臼齿)碳酸盐成因及其在元古宙地球演化中的意义. 岩石学报, 22(8): 2133-2143.
[Meng X H,Ge M,Kuang H W,Nielsen J K.2006. Origin of Microsparite carbonates and the significance in the evolution of the Earth in Proterozoic. Acta Petrologica Sinica, 22(8): 2133-2143]
[57] 孟祥化,葛铭,任国选,刘自亮,李现根,刘贺娟. 2011. 宇地系统场沉积响应范例: 蓟县系雾迷山巨旋回层序及节律. 地学前缘, 18(4): 107-122.
[Meng X H,Ge M,Ren G X,Liu Z L,Li X G,Liu H J.2011. The example of Cosmos-Earth System responses: The supercyclic sequence and rhythms of the Wumishan Sub-system of Jixian System. Earth Science Frontiers, 18(4): 107-122]
[58] 缪庆海,马艳平,付金沐,贾刚. 2014. 安徽灵璧地区张渠组臼齿构造成因分析. 宿州学院学报, 29(10): 79-84.
[Miao Q H,Ma Y P,Fu J M,Jia G.2014. The genesis analysis of the molar-tooth structures of the Zhangqu Formation in the Lingbi area,Anhui Province. Journal of Suzhou University, 29(10): 79-84]
[59] 彭楠,旷红伟. 2010. 辽东大连金石滩新元古代碳酸盐岩臼齿构造形态及其沉积环境指示意义. 岩石矿物学杂志, 29(2): 189-198.
[Peng N,Kuang H W.2010. Morphology of molar-tooth structures in Neoproterozoic and its indication significance for the depositional environment of Jinshitan area in Dalian,eastern Liaoning Province. Bulletin of Mineralogy,Petrology and Geochemistry, 29(2): 189-198]
[60] 彭楠,旷红伟,柳永清,李家华. 2010. 大连金石滩兴民村组臼齿碳酸盐岩及其沉积环境研究. 矿物岩石地球化学通报, 29(2): 127-133.
[Peng N,Kuang H W,Liu Y Q,Li J H.2010. Lithologic characteristics and sedimentary environment of molar-tooth carbonates in the Xingmincun Formation,Golden Pebble Beach region,Dalian. Bulletin of Mineralogy,Petrology and Geochemistry, 29(2): 127-133]
[61] 彭楠,柳永清,旷红伟. 2012. 沉积环境与臼齿构造(Molar-tooth)形态的关系: 以大连新元古代臼齿构造为例. 高校地质学报, 18(1): 180-188.
[Peng N,Liu Y Q,Kuang H W.2012. Relationship between depositional environment and morphology of molar tooth: Taking the Neoproterozoic molar-tooth in Dalian,China as an example. Geological Journal of China Universities, 18(1): 180-188]
[62] 乔秀夫,宋天锐,高林志,彭阳,李海兵,高劢,宋彪,张巧大. 1994. 碳酸盐岩振动液化地震序列. 地质学报, 68(1): 16-34.
[Qiao X F,Song T R,Gao L Z,Peng Y,Li H B,Gao M,Song B,Zhang Q D.1994. Seismic sequence in carbonate rocks by vibrational liquefaction. Acta Geologica Sinica, 68(1): 16-34]
[63] 乔秀夫,高林志,彭阳,章雨旭. 1997. 内蒙古腮林忽洞群综合地层和白云鄂博矿床赋矿微晶丘. 地质学报, 71(3): 202-211.
[Qiao X F,Gao L Z,Peng Y,Zhang Y X.1997. Composite stratigraphy of the sailinhudong Group and ore-braring micrite mound in the Bayan Obo deposit,Inner Monggolia,China. Acta Geologica Sinica, 71(3): 202-211]
[64] 乔秀夫,李海兵,苏德辰,何碧竹,田洪水,郭宪璞,宋天锐,吕洪波,高林志,贺静,袁效奇,周玮,张淼,孙爱萍,王安东. 2017. 软沉积物变形构造—地震与古地震记录. 北京: 地质出版社,1-264.
[Qiao X F,Li H B,Su D C,He B Z,Tian H S,Guo X P,Song T R,Lü H B,Gao L Z,He J,Yuan X Q,Zhou W,Zhang M,Sun A P,Wang A D. 2017. Soft Sediment Deformation Structures: Earthquake and Accient Earthquake Records. Beijing: Geological publishing house,1-264]
[65] 全国地层委员会. 2018. 中国岩石地层名词大全(上卷). 北京: 地质出版社,1-486.
[National Commission on Stratigraphy of China. A Complete Glossary of Rocks and Strata in China(PartⅠ). Beijing: Geological Publishing House,1-486]
[66] 田洪水,袁静,张慎河,魏焕卫,张邦花. 2006. 沂沭断裂带及其近区不同地质时期地震液化脉构造对比. 沉积学报, 24(4): 496-501.
[Tian H S,Yuan J,Zhang S H,Wei H W,Zhang B H.2006. The correlation of liquefied vein structures caused by earthquake in different geological periods in the Yishu fault zone and its vicinity. Acta Sedimentologica Sinica, 24(4): 496-501]
[67] 万渝生,刘敦一,王世炎,赵逊,董春艳,周红英,殷小艳,杨长秀,高林志. 2009. 登封地区早前寒武纪地壳演化—地球化学和锆石 SHRIMP U-Pb 年代学制约. 地质学报,83(7): 982-999.
[Wan Y S,Liu D Y,Wang S Y,Zhao X,Dong C Y,Zhou H Y,Yin X Y,Yang C X,Gao L Z.2009. Early Precambrian crustal evolution in the Dengfeng area,Henan Province(eastern China): Constraints from geochemistry and SHRIMP U-Pb zircon dating. Acta Geologica Sinica,83(7): 982-999]
[68] 王炳山,张宪依,李金波. 2007. 郯庐断裂带鲁南段新元古界石旺庄组的震积岩序列. 山东科技大学学报(自然科学版), 26(4): 4-9,22.
[Wang B S,Zhang X Y,Li J B.2007. Seismites sequence of Shiwangzhuang Formation of Neoproterozoic in South Shandong sector of Tancheng-Lujiang fault zone. Journal of Shandong University of Science and Technology(Natural Science), 26(4): 4-9,22]
[69] 王德海,郭峰,任国选,孟祥化,葛铭. 2004. 天津蓟县地区中元古代微亮晶碳酸盐岩的发现及其成因初探. 见: 第三届全国沉积学大会会议论文集. 成都: 47-48.
[Wang D H,Guo F,Ren G X,Meng X H,Ge M. 2004. The discovery of the Mesoproterozoic microspar carbonates in Jixian area,Tianjin,and its geological significance. In: 3th National Sedimentological Congress Proceedings. Chengdu: 47-48]
[70] 王德海,孟祥化,郭峰,任国选,葛铭. 2009. 天津蓟县高于庄组微亮晶(MT)碳酸盐岩的沉积环境及成因探讨. 吉林大学学报(地球科学版), 39(6): 1023-1030.
[Wang D H,Meng X H,Guo F,Ren G X,Ge M.2009. Discussion on the sedimentary environment and origin of the microsparite carbonates of Mesoproterozoic Gaoyuzhuang Formation in Jixian area,Tianjin,China. Journal of Jilin University(Earth Science Edition), 39(6): 1023-1030]
[71] 王泽九,沈其韩,万渝生. 2004. 河南登封石牌河“变闪长岩体”的锆石SHRIMP年代学研究. 地球学报,25(3): 295-298.
[Wang Z J,Shen Q H,Wan Y S.2004. SHRIMP U-Pb zircon geochronology of the Shipaihe “metadiorite mass”from Dengfeng Country,Henan Province. Acta Geoscientica Sinica,25(3): 295-298]
[72] 武振杰,张传恒,姚建新. 2009. 滇中中元古界大龙口组地震灾变事件及地质意义. 地球学报, 30(3): 375-386.
[Wu Z J,Zhang C H,Yao J X.2009. Neoproterozoic seismic catastrophic events in Dalongkou Formation of central Yunnan and their geological significance. Acta Geoscientica Sinica, 30(3): 375-386]
[73] 严兆彬,郭福生,彭花明,杨志,郭国林. 2005. 浙西寒武系大陈岭组地震事件沉积的初步研究. 地质学报, 79(6): 730-738.
[Yan Z B,Guo F S,Peng H M,Yang Z,Guo G L.2005. Pilot study on sedimentation of Cambrian Dachenling Formation resulting from seismic events in the west of Zhejiang Province. Acta Geologica Sinica, 79(6): 730-738]
[74] 严兆彬,郭福生,胡珺珺,刘礼洁. 2016. 浙西早寒武系大陈岭组地震液化脉电子探针分析研究. 煤炭工程, 48(11): 152-156.
[Yan Z B,Guo F S,Hu J J,Liu L J.2016. Electron microprobe analysis and seismic liquefied veins from the Early Cambrian Dachenling Formation in Western Zhejiang. Coal Engineering, 48(11): 152-156]
[75] 岳亮,刘自亮,李元敏. 2016. 微生物活动的沉积响应: 以MT构造为例. 地质科技情报, 35(6): 38-43.
[Yue L,Liu Z L,Li Y M.2016. Sedimentary response of microbial activities: A case study from MT structures. Geological Science and Technology Information, 35(6): 38-43]
[76] 翟明国,胡波,彭澎,赵太平. 2014. 华北中—新元古代的岩浆作用与多期裂谷事件. 地学前缘, 21(1): 100-119.
[Zhai M G,Hu B,Peng P,Zhao T P.2014. Meso-Neoproterozoic magmatic events and multi-stage rifting in the NCC. Earth Science Frontiers, 21(1): 100-119]
[77] 张邦花,田洪水,Wagoner Loon A J.2016. 新元古代沂沭海峡地震引发的软沉积物变形及其微量元素信息. 古地理学报, 19(1): 99-116.
[Zhang B H,Tian H S,Wagoner Loon A J.2016. Earthquake-induced soft sediment deformations and their trace-element information in the Neoproterozoic Yishu Strait. Journal of Palaeogeography(Chinese Edition), 19(1): 99-116]
[78] 张传恒,高林志,武振杰,史晓颖,阎全人,李大建. 2007. 滇中昆阳群凝灰岩锆石SHRIMP U-Pb年龄: 华南格林威尔期造山的证据. 科学通报, 52(7): 818-824.
[Zhang C H,Gao L Z,Wu Z J,Shi X Y,Yan Q R,Li D J.2007. Zircon SHRIMP U-Pb ages of tuff in the Kunyang Group in central Yunnan Province: Orogenic evidence for Grenville Period in South China. Chinese Science Bulletin, 52(7): 818-824]
[79] 张恒,高林志,周洪瑞,宋彪,丁孝忠,张传恒,刘昊岗,龚成强. 2019. 华北克拉通南缘官道口群和洛峪群的年代学研究新进展: 来自凝灰岩SHRIMP锆石U-Pb年龄的新证据. 岩石学报, 35(8): 2470-2486.
[Zhang H,Gao L Z,Zhou H R,Song B,Ding X Z,Zhang C H,Liu H G,Gong C Q.2019. Chronogy progress of the Guandaokou and Luoyu groups in the southern margin of North China Craton: Constraints on zircon U-Pb dating of tuff by means of the SHRIMP. Acta Petrologica Sinica, 35(8): 2470-2486]
[80] 周洪瑞,王自强,崔新省,雷振宇,董文明. 1998. 豫西地区中、新元古代地层沉积特征及层序地层学研究. 现代地质, 12(1): 17-24.
[Zhou H R,Wang Z Q,Cui X S,Lei Z Y,Dong W M.1998. Study on sedimentology and sequence stratigraphy of the Mesoproterozoic and Neoproterozoic in the west of Henan Province. Geoscience, 12(1): 17-24]
[81] Bishop J W,Sumner D Y,Huerta N J.2006. Molar tooth structures of the Neoarchean Monteville Formation,Transvaal Supergroup,South Africa. Ⅱ: A wave-induced fluid flow mode. Sedimentology, 53: 1069-1082.
[82] Bishop J W,Sumner D Y.2006. Molar tooth structures of the Neoarchean Montrvielle Formation,Transvaal supergroup,South Africa.: Constraints on microcrystalline CaCO₃ precipitation. Sedimentology, 53(5): 1049-1068.
[83] Fairchild I J,Einsele G,Song T R.1997. Possible seismic origin of molar tooth structures in Neoproterozoic carbonate ramp deposits,North China. Sedimentology, 44: 611-636.
[84] Fairchild I J,Spiro B,Herrington P M,Song T.2000. Controls on Sr and C isotope compositions of Neoproterozoic Sr-rich limestones of East Greenland and North China. SEPM Special Publication, 67: 297-313.
[85] Frank T D,Lyons T W.1998. “Molar-tooth”structures: A geochemical perspective on a Proterozoic enigma. Geology, 26(8): 683-686.
[86] Furniss G,Rittle J F,Winston D.1998. Gas bubble and expansion crack origin of “Molar-tooth”calcite structures in the Middle Proterozoic Belt supergroup western Montana. Journal of Sedimentary Research, 68(1): 104-114.
[87] Gao L Z,Zhang C H,Liu P J,Tang F,Song B,Ding X Z.2009. Reclassification of the Meso-and Neoproterozoic chronostratigraphy of North China by SHRIMP zircon ages. Acta Geologica Sinica, 83(6): 1074-1084.
[88] Ge M,Kuang H W,Meng X H,Furniss G.2004. Microorganisms linked to Neoproterozoic microspar carbonate sedimentation in the Jilin-Liaoning Area. Acta Geologica Sinica(English edition), 78(3): 784-789.
[89] Hodgskiss M S W,Kunzmann M,Poirier A,Halverson G P.2018. The role of microbial iron reduction in the formation of Proterozoic molar tooth structures. Earth and Planetary Science Letters, 482: 1-11.
[90] James N P,Narbonne G M,Sherman A G.1998. Molar tooth carbonate: Shallow subtidal facies of the Mid to Late Proterozoic. Journal of Sedimentary Research, 68(5): 716-722.
[91] Kuang H W,Li Y X,Zeng Y T,Meng X H,Ge M.2004. Biomarkers in the molar tooth(MT)-bearing limestones in the Jilin-Liaoning area of China. Chinese Journal of Geochemistry, 23(4): 334-341.
[92] Kuang H W,Liu Y X,Meng X H,Ge M.2007. A study on the environmental conditions of the microsparite(Molar-tooth)carbonates. Chinese Journal of Geochemistry, 26(1): 28-34.
[93] Kuang H W,Liu Y Q,Peng N,Luo S S,Li J H,Cen C,Chen M P.2012. Molar-Tooth Structure from the Mesoproterozoic Wumishan Formation in Lingyuan,Yanshan Region,North China,and Geological Implications. Acta Geologica Sinica(English Edition), 86(1): 85-95.
[94] Kuang H W.2014. Review of molar tooth structure research. Journal of Palaeogeography, 3(4): 359-383.
[95] Liu Y Q,Gao L Z,Liu Y X.2005. Neoproterozoic molar-tooth structure and constraint of depositional facies and environment in the North China Platform in Jiangsu,Anhui and Liaoning,eastern China. Acta Geologica Sinica(English Edition), 79(4): 533-539.
[96] Mei M X,Tucker M E.2011. Molar tooth structure: A contribution from the Mesoproterozoic Gaoyuzhuang Formation,Tianjin City,North China. Acta Geologica Sinica(English Edition), 85(5): 1084-1099.
[97] Meng X H,Ge M.2002. The sedimentary features of Proterozoic microspar(molar-tooth)carbonates in China and their significance. Episodes, 25(3): 185-196.
[98] Meng X H,Ge M.2003. Cyclic sequences,events and evolution of the Sino-Korean Plate,with a discussion on the evolution of Molar-tooth carbonates,phosphorites and source rocks. Acta Geologica Sinica(English edition), 77(3): 382-401.
[99] Meng X H,Ge M,Kuang H W,Cai G Y.2003. Recent advance in Precambrian carbonate sedimentary geology: Report on International Conference of IGCP447 on Molar Tooth Carbonates and Evolution of the Earth in the Proterozoic. Episodes, 26(1): 28-29.
[100] Meng X H,Ge M,Liu Y X,Kuang H W,Liu W F,Bourrouilh-LE Jan F G,Bourrouilh R.2004. Molar-tooth carbonate sequences and Sr isotopes in the Neoproterozoic for stratigraphic correlation: Research in the Jilin-Liaoning-Xuzhou-Huaiyang area of the Sino-Korean Plate and its correlation with the Yangtze Plate. Acta Geologica Sinica(English edition), 78(3): 775-783.
[101] O’Connor M P.1972. Classification and environmental interpretation of the cryptalgal organosedimentary“molar-tooth”structure from the late Precambrian Belt-Purcell Supergroup. Journal of Geology, 80(5): 592-610.
[102] Pollock M D,Kah L C,Bartley Julie K.2006. Morphology of molar-tooth structures in Precambrian carbonates: Influence of substrate rheology and implications for genesis. Journal of Sedimentary Research, 76: 310-323.
[103] Pope M C,Bartley J K,Knoll A H,Petrov P Y.2003. Molar tooth structures in calcareous nodules,early Neoproterozoic Burovaya Formation,Turukhansk region,Siberia. Sedimentary Geology, 158: 235-248.
[104] Pratt B R.1998. Molar-tooth structure in Proterozoic carbonate rocks: Origin from synsedimentary earthquakes and implication for the nature and evolution of basins and marine sediment. Geological Society of America Bulletin, 110(8): 1028-1045.
[105] Shanmugam G.2016. The seismite problem. Journal of Palaeogeography, 5(4): 318-362.
[106] Shen B,Dong L,Xiao S H,Lang X G,Huang K J,Peng Y B,Zhou C M,Ke S,Liu P J.2016. Molar tooth carbonates and benthic methane fluxes in Proterozoic oceans. Nature Communications, 7: 10317,DOI: 10.1038/ncomms10317.
[107] Shields G A.2002. “Molar-tooth microspar”: A chemical explanation for its disappearance-750 Ma. Terra Nova, 14: 108-113.
[108] Smith A G. 2016. A review of molar-tooth structures with some speculations on their origin. In: MacLean J S,Sears J W(eds).Belt Basin: Window to Mesoproterozoic Earth. Geological Society of America Special Paper, 522: 71-99.
[109] Wu H,Ding X Z,Liu Y X,Kuang H W.2017. New discovery of molar tooth structures in the Kangjia Formation at Benxi,Liaoning and its significance. Acta Geologica Sinica(English Edition), 91(3): 1139-1140.
[110] Zhao G,Cao L,Wilde S A,Sun M,Choe W J,Li S Z.2006. Implications based on the first SHRIMP U-Pb zircon dating on Precambrian granitoid rocks in North Korea. Earth and Planetary Science Letters, 251(3): 365-379.
[111] Zhao T P,Zhou M F. 2009. Geochemical constraints on the tectonic setting of Paleoproterozoic A-type granites in the southern margin of the North China Craton. Journal of Asian Earth Sciences,2009,36(2-3): 183-195.
[112] Zhou G T,Yao Q Z,Fu S Q,Guan Y B.2010. Controlled crystallization of unstable vaterite with distinct morphologies and their polymorphic transition to stable calcite. European Journal of Mineralogy, 22(2): 259-269.
[113] Zhou Y Y,Zhao T P,Wang CY,Hu G H.2011. Geochronology and geochemistry of 2.5 to 2.4 Ga granitic plutons in the southern margin of the North China Craton: Implications for a tectonic transition from arc to post-collisional setting. Gondwana Research,20(1): 171-183.

选择文件类型/文献管理软件名称

选择包含的内容

河南嵩山地区新元古界何家寨组微亮晶(臼齿)碳酸盐岩成因新认识^*

New understanding on the genetic mechanism of microsparite(molar-tooth)carbonates in the Neoproterozoic Hejiazhai Formation in Songshan area,Henan Province

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 4

编辑推荐

Metrics

本文评价

[1]	旷红伟, 彭楠, 王玉冲, 白华青, 祁柯宁, 柳永清. 臼齿碳酸盐岩: 解密前寒武纪海洋化学性质的钥匙^*[J]. 古地理学报, 2023, 25(1): 1-22.
[2]	旷红伟, 柳永清, 耿元生, 白华青, 彭楠, 范正秀, 宋换新, 夏晓旭, 王玉冲, 陈骁帅. 中国中新元古代重要沉积地质事件及其意义^*[J]. 古地理学报, 2019, 21(1): 1-30.
[3]	贾志海宁霄峰洪天求郑文武. 苏皖北部新元古界臼齿碳酸盐岩脉类型及其形成机理^*[J]. 古地理学报, 2011, 13(6): 627-634.
[4]	旷红伟, 柳永清, 彭楠, 刘燕学, 李家华. 再论臼齿碳酸盐岩成因^*[J]. 古地理学报, 2011, 13(3): 253-261.

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

河南嵩山地区新元古界何家寨组微亮晶(臼齿)碳酸盐岩成因新认识*

New understanding on the genetic mechanism of microsparite(molar-tooth)carbonates in the Neoproterozoic Hejiazhai Formation in Songshan area,Henan Province

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 4

编辑推荐

Metrics

本文评价

河南嵩山地区新元古界何家寨组微亮晶(臼齿)碳酸盐岩成因新认识^*