南极煤系地层特征及其对冈瓦纳大陆裂解的启示-岩石矿物学杂志-CSCIED科技核心评价数据库-手机版

南极煤系地层特征及其对冈瓦纳大陆裂解的启示

Stratigraphic distribution of coal measures in Antarctica and its implications for breakup of the Gondwana

ES评分 0 浏览量：324 下载量：0

DOI	10.20086/j.cnki.yskw.2025.4078
刊名	岩石矿物学杂志 Acta Petrologica et Mineralogica
年，卷(期)	2025, 44(2)
作者	张浩，崔迎春*，宗师，陈绍聪，马立杰，王伟轩，王雪娇，李升贵，刘晨光,
作者单位	1. 中国极地研究中心(中国极地研究所), 上海 200136; 2. 中国科学院海洋研究所中国科学院海洋地质与环境重点实验室, 山东青岛 266071; 3. 自然资源部第一海洋研究所海洋沉积与环境地质国家重点实验室, 山东青岛 266061
摘要	南极的煤系地层资源潜力巨大但研究十分有限。目前已发现的煤系地层主要为二叠纪地层,少量中、新生代地层,基本分布于横贯南极山脉及东南极查尔斯王子山脉地区,部分见于西南极。横贯南极山脉富煤地层主要为贝肯超群的二叠纪-三叠纪维多利亚群,查尔斯王子山脉富煤地层主要为埃默里群的二叠纪贝恩梅达特煤系。南极的煤具有高热阶特征,多为热变质煤。横贯南极山脉区域的煤多为无烟煤、超无烟煤或天然焦炭,具有高蚀变特征;查尔斯王子山脉区域的煤具有高挥发分低硫特征,贝恩梅达特煤系地层内随地层时代由老到新,代表煤系地层成熟度的镜质体反射率呈逐步降低至相对稳定趋势。南极主要煤系地层的发育揭示晚古生代-早中生代时期,南极温暖湿润、植被繁茂,沉积环境与如今存在巨大差异,现存煤系地层多发育于河、湖相沉积交错处。煤系地层发育热演化史揭示,南极热变质煤系地层的形成与冈瓦纳大陆裂解有关,弗拉尔大火山岩省沿横贯南极山脉的线性分布特征与典型二叠纪煤系地层分布特征耦合,侏罗纪短期集中热事件形成的岩脉侵入可以作为煤系地层热蚀变开始的信号,白垩纪末的冈瓦纳大陆进一步裂解形成的热升温,可能是导致南极煤系地层呈现高煤阶、高成熟度的主因。
Abstract	The coal measure resources in Antarctica possess great potential yet have received limited research. The discovered coal measures are predominantly Permian strata, with a few being Mesozoic-Cenozoic strata. The coal measures are essentially distributed in the Transantarctic Mountains and Prince Charles Mountains, with some parts found in West Antarctica. The coal-abundant strata in the Transantarctic Mountains are mainly Permian-Triassic Victoria Group of the Bacon Supergroup, and the coal-abundant strata in the Prince Charles Mountains are mainly Permian Bainmedart Coal Measures of the Amery Group. The coal in Antarctica exhibits the characteristics of a high thermal order and is mostly thermal metamorphic coal. The coal in the Transantarctic Mountains is mostly anthracite, super anthracite, or natural coke, which has the characteristics of high alteration. The coal in the Prince Charles Mountains region has the characteristics of high volatility and low sulfur. The vitrinite reflectance, which represents the maturity of coal measures, gradually decreases to a relatively stable trend as the formation age from old to new in the Bainmedart Coal Measures. The development of major coal measures in Antarctica reveals that during the Late Paleozoic and Early Mesozoic, the Antarctic was warm and humid with lush vegetation, and the sedimentary environment was vastly different from that of today. The existing coal measures were mostly developed at the intersection of river and lake sedimentary facies. The development and history of the thermal evolution of coal measure disclose that the formation of Antarctic thermal metamorphic coal measure is related to the breakup of Gondwana. The linear distribution along the Transantarctic Mountains of the Ferrar Large Igneous Province is coupled with the location of typical Permian coal measures, and the dike formed by the Jurassic short-term concentrated thermal event can be regarded as the signal of the commencement of thermal alteration of the coal measure, while the heat rise caused by the further breakup of Gondwana at the end of Cretaceous may be the main cause of the high coal rank and high maturity of the Antarctic coal measure.
关键词	南极；二叠纪；煤系地层；岩相古地理；热演化史；冈瓦纳裂解
KeyWord	Antarctica; Permian; coal measure; lithofacies paleogeography; thermal evolution history; Gondwana breakup
基金项目
页码	438-450

参考文献
相关文献

Awatar R, Tewari R, Agnihotri D, et al. 2014. Late Permian and Triassic palynomorphs from the Allan Hills, central Transantarctic Mountains, South Victoria Land, Antarctica
[J]. Current Science, 988~996. Barker P F. 1982. The Cenozoic subduction history of the Pacific margin of the Antarctic Peninsula: Ridge crest-trench interactions
[J]. Journal of the Geological Society, 139(6): 787~801. Barker P F and Burrell J. 1977. The opening of Drake passage
[J] . Marine Geology, 25(1~3): 15~34. Barrett P J. 1965. Geology of the area between the Axel Heiberg and Shackleton Glaciers, Queen Maud Range, Antarctica: Part 2—Beacon group
[J]. New Zealand Journal of Geology and Geophysics, 8(2): 344~363. Barrett P J, Elliot D H and Lindsay J F. 1986. The Beacon Supergroup (Devonian-Triassic) and Ferrar Group (Jurrasic) in the Beardmore Glacier Area, Antarctica
[J]. Geology of the Central Transantarctic Mountains, 36: 339~428. Bauer W. 1997. Permian Coals from Western Dronning Maud Land-Composition, Environment, and the Influence of Jurassic Magmatism on their Maturity
[C]//Ricci C A. The Antarctic Region, Geological Evolution and Processes. Proceedings of the VII International Symposium on Antarctic Earth Sciences Terra Antartica Publication, Siena, 945~951. Bauer W. 2009. Permian sedimentary cover, Heimefrontfjella, western Dronning Maud Land (East Antarctica)
[J]. Polarforschung, 79(1): 39~42. Behrendt J C and Cooper A. 1991. Evidence of rapid Cenozoic uplift of the shoulder escarpment of the Cenozoic West Antarctic rift system and a speculation on possible climate forcing
[J]. Geology, 19(4): 315~319. Birkenmajer K, Frankiewicz J K and Wagner M. 1991. Tertiary coal from the Lions Cove Formation, King George Island, West Antarctica
[J]. Polish Polar Research,12(2): 229~241. Black L P, Williams I S and Compston W. 1986. Four zircon ages from one rock: The history of a 3 930 Ma-old granulite from Mount Sones, Enderby Land, Antarctica
[J]. Contributions to Mineralogy and Petrology, 94(4): 427~437. Bomfleur B, Schöner R, Schneider J W, et al. 2014. From the Transantarctic Basin to the Ferrar Large Igneous Province—New palynostratigraphic age constraints for Triassic-Jurassic sedimentation and magmatism in East Antarctica
[J]. Review of Palaeobotany and Palynology, 207: 18~37. Bostick N H, Cashman S M, McCulloh T H, et al. 1978. Gradients of vitrinite reflectance and present temperature in the Los Angeles and Ventura basins, California
[J]. Pacific, 65~96. Bradshaw M A. 2013. The Taylor Group (Beacon Supergroup): The Devonian sediments of Antarctica
[J]. Geological Society, London, Special Publications, 381(1): 67~97. Burgess S D, Bowring S A, Fleming T H, et al. 2015. High-precision geochronology links the Ferrar large igneous province with early-Jurassic ocean anoxia and biotic crisis
[J]. Earth and Planetary Science Letters, 415: 90~99. Chatterjee S, Tewari R and Agnihotri D. 2013. A Dicroidium flora from the Triassic of Allan hills, south Victoria Land, Transantarctic Mountains, Antarctica
[J]. Alcheringa: An Australasian Journal of Palaeontology, 37(2): 209~221. Chen Tingyu, Li Guangcen, Xie Liangzhen, et al. 1995. Geological Map of Antarctica (1∶5 000 000)
[M]. Beijing: Geological Publishing House (in Chinese). Coates D A, Stricker G D and Landis E R. 1990. Coal geology, coal quality, and coal resources in Permian rocks of the Beacon Supergroup, Transantarctic Mountains, Antarctica
[J]. Mineral Resources Potential of Antarctica, 51: 133~162. Collinson J W, Hammer W R, Askin R A, et al. 2006. Permian-Triassic boundary in the central transantarctic Mountains, Antarctica
[J]. Geological Society of America Bulletin, 118(5~6): 747~763. Collinson J W, Isbell J L, Elliot D H, et al. 1994. Permian-Triassic Transantarctic basin
[J]. Geological Society of America Memoirs, 184: 173~222. Cooper R A, Landis C A, LeMasurier W E, et al. 1982. Geologic history and regional patterns in New Zealand and West Antarctica—Their paleotectonic and paleogeographic significance
[J]. Antarctic Geoscience, 43~53. Cridland A A. 1963. A Glossopteris flora from the Ohio range, Antarctica
[J]. American Journal of Botany, 50(2): 186~195. Crohn P W. 1959. A Contribution to the Geology and Glaciology of the Western Part of Australian Antarctic Territory
[M]. Antarctic Division, Department of External Affairs. Dalziel I W D. 1983. The evolution of the Scotia Arc: A review
[J] . Antarctic Earth Science, 283~288. Elliot D H. 2013. The geological and tectonic evolution of the Transantarctic Mountains: A review
[J] . Geological Society, London, Special Publications, 381(1): 7~35. Elliot D H, Fanning C M, Isbell J L, et al. 2017. The Permo-Triassic Gondwana sequence, central Transantarctic Mountains, Antarctica: Zircon geochronology, provenance, and basin evolution
[J]. Geosphere, 13(1): 155~178. Elliot D H, Fanning C M and Laudon T S. 2016. The Gondwana plate margin in the Weddell Sea sector: Zircon geochronology of upper Paleozoic (mainly Permian) strata from the Ellsworth Mountains and eastern Ellsworth Land, Antarctica
[J]. Gondwana Research, 29(1): 234~247. Elliot D H and Fleming T H. 2008. Physical volcanology and geological relationships of the Jurassic Ferrar large igneous province, Antarctica
[J]. Journal of Volcanology and Geothermal Research, 172(1~2): 20~37. Elliot D H and Fleming T H. 2018. The Ferrar Large Igneous Province: Field and geochemical constraints on supra-crustal (high-level) emplacement of the magmatic system
[J]. Geological Society London Special Publications, 463: 41~58. Elliot D H and Fleming T H. 2021. Ferrar Large Igneous Province: Petrology
[J]. Geological Society London Memoirs, 55: 93~119. Elliot D H, Fleming T H, Kyle P R, et al. 1999. Long-distance transport of magmas in the Jurassic Ferrar large igneous province, Antarctica
[J]. Earth and Planetary Science Letters, 167(1~2): 89~104. Elliot D H, White J D L and Fleming T H. 2021. Ferrar Large Ugneous Province: Volcanology
[J]. Geological Society London Memoirs, 55: 79~91. Faure G and Mensing T M. 2010. The Transantarctic Mountains: Rocks, Ice, Meteorites and Water
[M]. Springer Science and Business Media. Fielding C R and Webb J A. 1995. Sedimentology of the Permian Radok Conglomerate in the Beaver Lake area of MacRobertson Land, East Antarctica
[J]. Geological Magazine, 132(1): 51~63. Fitzgerald P G. 1994. Thermochronologic constraints on post-Paleozoic tectonic evolution of the central Transantarctic Mountains, Antarctica
[J]. Tectonics, 13(4): 818~836. Holdgate G R, McLoughlin S, Drinnan A N, et al. 2005. Inorganic chemistry, petrography and palaeobotany of Permian coals in the Prince Charles Mountains, East Antarctica
[J]. International Journal of Coal Geology, 63(1~2): 156~177. Isbell J L and Cúneo N R. 1996. Depositional framework of Permian coal-bearing strata, southern Victoria Land, Antarctica
[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 125(1~4): 217~238. Kumar K, Chatterjee S, Tewari R, et al. 2013. Petrographic evidence as an indicator of volcanic forest fire from the Triassic of Allan Hills, South Victoria Land, Antarctica
[J]. Current Science, 104(4): 422~424. Kumar M, Tewari R, Chatterjee S, et al. 2011. Charcoalified plant remains from the Lashly Formation of Allan Hills, Antarctica: Evidence of forest fire during the Triassic Period
[J]. Episodes Journal of International Geoscience, 34(2): 109~118. Li K, Rimmer S M and Liu Q. 2018. Geochemical and petrographic analysis of graphitized coals from Central Hunan, China
[J]. International Journal of Coal Geology, 195: 267~279. Lindström S and McLoughlin S. 2007. Synchronous palynofloristic extinction and recovery after the end-Permian event in the Prince Charles Mountains, Antarctica: Implications for palynofloristic turnover across Gondwana
[J]. Review of Palaeobotany and Palynology, 145(1~2): 89~122. Long W E. 1965. Stratigraphy of the Ohio Range, Antarctica
[J]. Geology and Paleontology of the Antarctic, 6: 71~116. Ma Lijie, Liu Chenguang, Cui Yingchun, et al. 2018. Coal petrography and coal chemistry characteristics of Bainmedart Coal Measures, Northern Prince Charles Mountains
[J]. Journal of China Coal Society, 43(S1): 245~252 (in Chinese with English abstract). McLoughlin S. 2001. The breakup history of Gondwana and its impact on pre-Cenozoic floristic provincialism
[J]. Australian Journal of Botany, 49(3): 271~300. McLoughlin S and Drinnan A N. 1997a. Fluvial sedimentology and revised stratigraphy of the Triassic Flagstone Bench Formation, northern Prince Charles Mountains, East Antarctica
[J]. Geological Magazine, 134(6): 781~806. McLoughlin S and Drinnan A N. 1997b. Revised stratigraphy of the Permian Bainmedart Coal Measures, northern Prince Charles Mountains, East Antarctica
[J]. Geological Magazine, 134(3): 335~353. Merrill M D. 2016. GIS Representation of Coal-Bearing Areas in Antarctica
[M]. US Department of the Interior, US Geological Survey. Molzahn M, Wörner G, Henjes-Kunst F, et al. 1999. Constraints on the Cretaceous thermal event in the Transantarctic Mountains from alteration processes in Ferrar flood basalts
[J]. Global and Planetary Change, 23(1~4): 45~60. Pandita S K, Siddaiah N S, Tewari R, et al. 2018. Geochemistry of coal-bearing Permo-Triassic strata in Allan Hills, South Victoria Land, Antarctica: Implications for palaeoclimate
[J]. The Palaeobotanist, 67: 89~97. Pearson J and Murchison D. 1999. Relationship between reflectance and volatile-matter yield at the Maudlin (H) horizon of the offshore Northumberland and Durham coalfields
[J]. Fuel, 78(12): 1 417~1 423. Presswood S M, Rimmer S M, Anderson K B, et al. 2016. Geochemical and petrographic alteration of rapidly heated coals from the Herrin (No. 6) Coal Seam, Illinois Basin
[J]. International Journal of Coal Geology, 165: 243~256. Rahman M W, Rimmer S M, Rowe H D, et al. 2017. Carbon isotope analysis of whole-coal samples and vitrinite fractions from intruded coals from the Illinois Basin: No isotopic evidence for thermogenic methane generation
[J]. Chem. Geol., 453: 1~11. Retallack G J, Jahren A H, Sheldon N D, et al. 2005. The Permian-Triassic boundary in Antarctica
[J]. Antarctic Science, 17(2): 241~258. Rimmer S M, Yoksoulian L E and Hower J C. 2009. Anatomy of an intruded coal, I: Effect of contact metamorphism on whole-coal geochemistry, Springfield (No.5) (Pennsylvanian) coal, Illinois Basin
[J]. International Journal of Coal Geology, 79(3): 74~82. Rose G and Mcelroy C T. 1987. Coal potential of antarctica
[J]. Resource Report, Australia Bureau of Mineral Resources, Geology and Geophysics, 2: 1~19. Sanders M M and Rimmer S M. 2020. Revisiting the thermally metamorphosed coals of the Transantarctic Mountains, Antarctica
[J]. International Journal of Coal Geology, 228: 103550. Sanders M M, Rimmer S M and Rowe H D. 2023. Carbon isotopic composition and organic petrography of thermally metamorphosed Antarctic coal: Implications for evaluation of δ¹³C_org excursions in paleo-atmospheric reconstruction
[J]. International Journal of Coal Geology, 267: 104182. Schapiro N and Gray R J. 1966. Physical Variations in Highly Metamorphosed Antarctic Coals
[M]. American Chemical Society. Schopf J M. 1962. A preliminary report on plant remains and coal of the sedimentary section in the central range of the Horlick Mountains, Antarctica
[R]. Research Foundation and the Institute of Polar Studies, The Ohio State University. Schopf J M and Long W E. 1966. Coal Metamorphism and Igneous Associations in Antarctica
[M]. American Chemical Society. Snyman C P and Barclay J. 1989. The coalification of South African coal
[J]. International Journal of Coal Geology, 13(1~4): 375~390. Splettstoesser J F. 1980. Coal in Antarctica
[J]. Economic Geology, 75: 936~942. Talarico F, Ghezzo C and Kleinschmidt G. 2022. The Antarctic Continent in Gondwana: A Perspective from the Ross Embayment and Potential Research Targets for Future Investigations
[M]. Antarctic Climate Evolution, Elsevier, 219~296. Temminghoff M, Kruetzmann N, Danninger M, et al. 2007. Minerals Under Ice How far do we go to utilize Antarctic resources?
[R]. University of Canterbury, NZ. GCAS Syndicate Report 06/07. Tewari R, Chatterjee S, Agnihotri D, et al. 2015. Glossopteris flora in the Permian Weller Formation of Allan Hills, South Victoria Land, Antarctica: Implications for paleogeography, paleoclimatology, and biostratigraphic correlation
[J]. Gondwana Research, 28(3): 905~932. Veevers J J and Eittreim S L. 1988. Reconstruction of Antarctica and Australia at breakup (95±5 Ma) and before rifting (160 Ma)
[J]. Australian Journal of Earth Sciences, 35(3): 355~362. Yaxley G M, Kamenetsky V S, Nichols G T, et al. 2013. The discovery of kimberlites in Antarctica extends the vast Gondwanan Cretaceous province
[J]. Nature Communications, 4(1): 2 921. Zhu Jiangang, Yan Qide and Ling Xiaoliang. 2005. The analysis of Antarctic resources and their exploitation and potential utilization
[J]. China Soft Science, 8(10): 17~22 (in Chinese with English abstract). 附中文参考文献陈廷愚, 李光岑, 谢良珍, 等. 1995. 南极洲地质图(1∶5 000 000)
[M]. 北京: 地质出版社. 马立杰, 刘晨光, 崔迎春, 等. 2018. 北查尔斯王子山贝恩梅达特煤系煤层的煤岩学与煤化学特征
[J]. 煤炭学报, 43(S1): 245~252. 朱建钢, 颜其德, 凌晓良. 2005. 南极资源及其开发利用前景分析
[J]. 中国软科学, 8(10): 17~22.

引用本文

张浩，崔迎春*，宗师，陈绍聪，马立杰，王伟轩，王雪娇，李升贵，刘晨光. 南极煤系地层特征及其对冈瓦纳大陆裂解的启示 [J]. 岩石矿物学杂志. 2025; 44; (2). 438 - 450.

文献评论

相关学者

相关机构