nav emailalert searchbtn searchbox tablepage yinyongbenwen piczone journalimg journalInfo journalinfonormal searchdiv searchzone qikanlogo popupnotification paper paperNew
2025, 06, v.40 27-40
花岗岩与地震
基金项目(Foundation): 国家科技重大专项:深地特深科学钻探选址研究(2024ZD1001003); 自然资源部深地科学与探测技术实验室开放课题:下地壳底部填图理论与方法探索(202211); 国家重点研发计划项目:基于地质云的地质灾害基础信息提取与大数据分析挖掘(2018YFC1505501); 中国地质调查局项目:地球科学大数据“一张图”体系建设与知识服务(DD20230761); 中铁第一勘察设计院集团有限公司项目:地质信息数字化平台研发与应用示范(2021-A02); 邢台市科技局项目:沙河中关邯邢式铁矿碳酸盐同位素记录的温度信息(2023ZZ082)
邮箱(Email):
DOI:
摘要:

地震成因与花岗岩侵位及热力学过程密切相关。花岗岩侵位可引发三类地震:垮塌地震(岩浆房置换导致围岩失稳)、伸展地震(穹窿构造诱发正断层活动)和爆炸地震(超临界流体相变引发隐爆)。其中,爆炸地震因流体相变释放巨大能量,成为浅源破坏性地震的主因。通过厘清岩浆热场、流体运移和超临界流体相变与地震类型之间的关联性,强调爆炸地震机制研究对完善地震理论及其预测的关键意义,为解释唐山、汶川等大地震成因提供了新视角。

Abstract:

The genesis of earthquakes is closely related to granite intrusion and thermodynamic processes. This article proposes that granite intrusion can trigger three types of earthquakes: collapse earthquakes(rock instability caused by magma chamber displacement), extensional earthquakes(normal fault activity induced by dome structures), and explosive earthquakes(hidden explosions caused by supercritical fluid phase transitions). Among them, explosive earthquakes release enormous energy due to fluid phase transitions, becoming the main cause of shallow source destructive earthquakes. This article clarifies the correlation between magma thermal field, fluid migration, supercritical fluid phase transitions and earthquake types, emphasizing the key significance of studying explosive earthquake mechanisms for improving earthquake theory and prediction, and providing a new perspective for explaining the causes of major earthquakes such as Tangshan and Wenchuan earthquakes.

参考文献

[1] REID H F.The California earthquake of April 18,1906.Volume II.The mechanics of the earthquake[M].Washington DC:Carnegie Institution of Washington,Publication,1910,87:1-192.

[2] 松泽武雄.地震理论及其应用[M].黄兴建,唐贤书,译.北京:地震出版社,1980.

[3] 宋春青,邱维理,张振青.地质学基础[M].4版.北京:高等教育出版社,2005.

[4] 徐常芳.地震流体成因说及其应用研究[J].地震,1998(增刊1):89-97.

[5] 杜建国.地球深部流体和孕震介质研究进展[J].地震监测,1999(3):92-96.

[6] 梁光河.从汶川地震探讨隐爆与成矿过程[J].岩石学报,2017(2):326-338.

[7] 江建富.地震成因新说[M]//王优龙.减灾趣闻启示录.北京:地震出版社,1994:1-82.

[8] 张宝盈.地震电磁成因假说[J].高原地震,2005(2):1-21.

[9] 曾雄飞.地震结构爆裂动力学理论[J].广东科技,2010(增刊1):16-20.

[10] 曾雄飞.汶川地震引领爆裂动力学理论发展[J].广东科技,2010(2):202-204.

[11] 杨巍然,曾佐勋,李德威,等.板内地震过程的三层次构造模式[J].地学前缘,2009(1):206-217.

[12] 岳中琦.汶川地震与山崩地裂的极高压甲烷天然气成因和机理[J].地学前缘,2013(6):15-20.

[13] 梁光河.地震与成矿过程研究综述[J].黄金科学技术,2016(6):8-14.

[14] 曾佐勋,陈志耕,鲁成东,等.地震机理的地球系统科学研究及预测实践[J].地学前缘,2021(6):263-282.

[15] 陈运泰,吴忠良,吕苑苑.地震的分类[J].城市与减灾,2003(1):1-13.

[16] 杜建国,仵柯田,孙凤霞,等.隐爆角砾岩:古地震的一种成因标志[J].岩石学报,2022(3):913-922.

[17] NOPPE M G.The chemical channel of earthquake reactions and decrease in the magnitude of earthquakes[J].International journal of geosciences,2020,11(3):84-99.

[18] 张旗,原杰,焦守涛,等.构造地震还是爆炸地震?[J].邢台学院学报,2025(2):23-39.

[19] 李绍柄.唐山地震的发震构造与成因的探讨[J].华北地震科学,1986(2):56-62.

[20] 刘武英,李龙海,吴建华,等.从地球化学角度讨论1976年唐山7.8级地震的成因[J].地质地球化学,1996(5):66-69.

[21] 陈立德,付虹.汶川8.0级地震前兆异常对比研究[J].内陆地震,2010(4):289-297.

[22] 陈立德,付虹,张翔,等.地震力学成因及前兆机理研究:再“读” 唐山地震有感[J].地震研究,2019(1):1-10.

[23] 徐常芳.深部流体在地震孕育和发生过程中的作用[J].华南地震,2002(3):1-10.

[24] 徐常芳.中国大陆壳内与上地幔高导层成因及唐山地震机理研究[J].地学前缘,2003(增刊1):101-111.

[25] 曾融生,张少泉,周海南,等.唐山地震区的地壳结构及大陆地震成因的探讨[J].地震学报,1985(2):125-142.

[26] 曾融生,陆涵行,丁志峰.从地震折射和反射剖面结果讨论唐山地震成因[J].地球物理学报,1988(4):383-398.

[27] 曾融生,朱露培,何正勤,等.华北盆地强震的震源模型兼论强震和盆地的成因[J].地球物理学报,1991(3):288-301.

[28] 赵慈平,陈有丽,王云,等.云南宁洱-通关火山区最上地壳地热场:构造和岩浆活动意义[J].岩石学报,2014(12):3645-3656.

[29] 白思胜.隐爆地震[J].灾害学,2004(3):92-96.

[30] 陈志耕.东秦岭216.8 Ma前7.0级隐爆成因大地震的震源遗迹[J].地质学报,2015(8):1495-1529.

[31] 赵文平,赵强,王侃.试论秦岭造山带巨型隐爆角砾岩带与古地震及成矿之关系[J].陕西地质,2023(2):97-104.

[32] 张旗,钟涛,原杰,等.爆炸地震理论概述[J].邢台学院学报,2025(4):28-43.

[33] SPEERS E C.The age relation and origin of common Sudbury breccia[J].The journal of geology,1957,65(5):497-514.

[34] WRIGHT A E,BOWES D R.Formation of explosion-breccias[J].Bulletin volcanologique,1968,32(1):15-32.

[35] OFFICER C B,CARTER N L.A review of the structure,petrology,and dynamic deformation characteristics of some enigmatic terrestrial structures[J].Earth-science reviews,1991,30(1/2):1-49.

[36] LAZNICKA P.Breccias and ores.part 1:history,organization and petrography of breccias[J].Ore geology reviews,1989,4(4):315-344.

[37] JéBRAK M.Hydrothermal breccias in vein-type ore deposits:a review of mechanisms,morphology and size distribution[J].Ore geology reviews,1997,12(3):111-134.

[38] XU X W,CAI X P,QIN D J,et al.Fluids double-fracturing genetic mechanism and mineralization of gold-copper of the breccia pipe at Qibaoshan in Shandong Province[J].Science in China series D:earth sciences,2000,43(2):113-121.

[39] 卿敏,韩先菊.隐爆角砾岩型金矿研究述评[J].黄金地质,2002(2):1-7.

[40] ROSS P S,JEBRAK M,WALKER B M.Discharge of hydrothermal fluids from a magma chamber and concomitant formation of a stratified breccia zone at the questa porphyry molybdenum deposit,new Mexico[J].Economic geology,2002,97(8):1679-1699.

[41] COX S F,RUMING K.The St Ives mesothermal gold system,western Australia:a case of golden aftershocks?[J].Journal of structural geology,2004,26(6/7):1109-1125.

[42] LAUGHTON J R,THORKELSON D J,BRIDEAU M A,et al.Early Proterozoic orogeny and exhumation of Wernecke Supergroup revealed by vent facies of Wernecke Breccia,Yukon,Canada[J].Canadian journal of earth sciences,2005,42(6):1033-1044.

[43] LI N,CARRANZA E J M,NI Z Y,et al.The CO2-rich magmatic-hydrothermal fluid of the Qiyugou breccia pipe,Henan Province,China:implication for breccia genesis and gold mineralization[J].Geochemistry:exploration,environment,analysis,2012,12(2):147-160.

[44] CRAW D.Gilded by earthquakes[J].Nature geoscience,2013,6(4):248-250.

[45] GAO L,ZENG L S,ASIMOW P D.Contrasting geochemical signatures of fluid-absent versus fluid-fluxed melting of muscovite in metasedimentary sources:the Himalayan leucogranites[J].Geology,2017,45(1):39-42.

[46] 章增凤.隐爆角砾岩的特征及其形成机制[J].地质科技情报,1991(4):1-5.

[47] DAVIES A G S,COOKE D R,GEMMELL J B,et al.Hydrothermal breccias and veins at the Kelian Gold Mine,Kalimantan,Indonesia:genesis of a large epithermal gold deposit[J].Economic geology,2008,103(4):717-757.

[48] CAS R,GIORDANO G,BALSAMO F,et al.Hydrothermal breccia textures and processes:Lisca Bianca islet,Panarea Volcano,Aeolian Islands,Italy[J].Economic geology,2011,106(3):437-450.

[49] SAGE R P.Diatremes and shock features in Precambrian rocks of the Slate Islands,northeastern Lake Superior[J].GSA Bulletin,1978,89(10):1529-1540.

[50] 王照波.隐爆岩及其形成模式探讨[J].地质找矿论丛,2001(3):201-205.

[51] 宁建国,宋卫东,任会兰,等.冲击载荷作用下材料与结构的响应与防护[J].固体力学学报,2010(5):532-552.

[52] 梁光河.地震新知[J].百科知识,2016(14):4-11.

[53] 汤懋苍,董文杰.地气耦合研究进展简介[J].地球物理学进展,1993(1):60-67.

[54] 张旗,金惟浚,李承东,等.“岩浆热场” 说及其成矿意义:上[J].甘肃地质,2014(1):1-18.

[55] 张旗,金惟浚,李承东,等.“岩浆热场” 说及其成矿意义:下[J].甘肃地质,2014(2):1-20.

① 该示例图片取自网络,原图为三维立体图。示例图片删除了原图中三维立体信息和水印,仅保留了地层内部关键的坍塌情况。原图地址:http://www.360doc.com/content/18/0228/22/3046928_733288259.shtml

基本信息:

中图分类号:P588.121;P315

引用信息:

[1]张旗,钟涛,李承东,等.花岗岩与地震[J].邢台学院学报,2025,40(06):27-40.

基金信息:

国家科技重大专项:深地特深科学钻探选址研究(2024ZD1001003); 自然资源部深地科学与探测技术实验室开放课题:下地壳底部填图理论与方法探索(202211); 国家重点研发计划项目:基于地质云的地质灾害基础信息提取与大数据分析挖掘(2018YFC1505501); 中国地质调查局项目:地球科学大数据“一张图”体系建设与知识服务(DD20230761); 中铁第一勘察设计院集团有限公司项目:地质信息数字化平台研发与应用示范(2021-A02); 邢台市科技局项目:沙河中关邯邢式铁矿碳酸盐同位素记录的温度信息(2023ZZ082)

检 索 高级检索