共查询到17条相似文献,搜索用时 171 毫秒
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在野外考察、室内分析的基础上对清平飞来峰的构造特征、形成机制进行了研究。其结果表明清平飞来峰具有明显的叠覆式特征,共分5层。各层峰体特征、成因各具特色,下部两层为推覆体,上部三层为滑覆体。推覆体与滑覆体共同构成同一飞来峰,为龙门山飞来峰中所少见。从而证实了龙门山飞来峰先发育推覆体,后发育滑覆体的地质景观确实存在。 相似文献
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龙门山彭州—什邡地区的巨型冰川漂砾 总被引:6,自引:1,他引:5
论述了塘坝子等地的“飞来峰”是由汶川搬运到喜州等地来的巨型冰川漂砾,同时分析了“飞来峰”石灰岩呈角砾状是由冰劈作用和厚层冰雪压碎作用,再经胶结的结果,提出了冰冻灰岩这一词语。 相似文献
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龙门山南段大型飞来峰 总被引:10,自引:1,他引:9
最近1∶5×104区调查明的白石-苟家大型飞来峰,面积达320km2,其规模仅次于唐王寨飞来峰,由泥盆系养马坝组至三叠系嘉陵江组构成,准原地系统为上三叠统须家河组及侏罗系红层。飞来峰主体构造为向斜,两翼不对称,内部构造的规律性和运动学特征表明它是由NW方向滑来。飞来峰体具多层结构,在其就位后又受到晚期挤压的改造。其主要特征与唐王寨构造极为相似。飞来峰的成因研究对龙门山的构造演化具有重要意义。 相似文献
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(一)前言鹤庆锰矿位于鹤庆县城西南小水井一带,是一低磷、低铁、自熔性中型规模的富锰矿床。自五十年代开展地质工作以来,对矿床成因、含矿地层时代、沉积环境、成矿远景等作过论述和探讨,一致认为含锰地层为上三叠统松桂组。但这是一个还未理清楚的问题。在1:20万鹤庆幅区测报告验收决议书中指出,矿区的马厂东山一带,作为“飞来峰”构造的中三叠统北衙组缺乏确切的化石依据,定为“飞来峰”和推覆构造的资料不够充分。笔者自六十年代初至今,一直参与了该区的区调工作,对黑泥哨以北、汝南哨以南一带包括含锰地层在内的一套碎屑岩、火山岩、火山碎屑岩及碳酸盐岩进行了系统的剖面观察,采集到不少化石。现在认为,原先定的“飞来峰”构造是不存在的,下面的含锰碎屑岩与其上的碳酸盐岩 相似文献
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龙门山造山带以发育飞来峰构造为国内外地质学者所瞩目,前人对其进行了较为深入的研究,并取得了卓越的成果,但是对飞来峰的性质、成因机制和形成演化等重大地质问题仍存在较大争议。本文基于广元三堆地区区域地质调查、室内资料分析整理,对飞来峰构造进行研究。认为三堆地区飞来峰构造是由NW向SE方向逆冲推覆岩片形成。飞来峰具有"多层楼式"结构,其中三门垭下层飞来峰体以谢家沟断层(F3)为主滑动面的推覆体为根带,形成时代明显比上层飞来峰体更早,发育时间应该在前燕山期,并经历后期喜山运动的改造。以泥盆系等地层组成的飞来峰体根带被梨树坝断层(F1)掩盖,形成时间为喜山期,与山前磨拉石(大邑砾岩)堆积时期同期,即上新世(N2)-早更新世(Q1)。 相似文献
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晏家铺向斜位于湖南省涟源县城以北 ,涟邵煤田北段中部 ,由石炭系、二叠系、三叠系等地层组成。向斜形似纺缍 ,轴向NE35°左右 ,两翼发育一些飞来峰构造(图略)。本区的飞来峰构造按其成因可分两类 :推覆类型和滑覆类型。1推覆类型的飞来峰构造西北翼杨家山勘探区的朱家凼飞来峰(图1)及鲫鱼塘飞来峰。其形成机制是由于集云断层由东向西将测水组(C1c)推覆在壶天群(C2 3)灰岩之上 ,再遭侵蚀作用而形成的。这种类型的飞来峰是比较常见的传统类型。是老地层在新地层之上 ,具有老压新的特点。2滑覆类型的飞来峰构造在南翼有… 相似文献
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龙门山国家地质公园飞来峰成因的新证据 总被引:1,自引:0,他引:1
近来发现四川彭州(原称彭县)、什邡一带的飞来峰是第四纪冰川作用形成的。笔者等在塘坝子、葛仙山等飞来峰的底界及周边,多次发现飞来峰是压在早更新世的冰水堆积层之上。葛仙山北寨门、丁家湾,什邡大垭口等剖面的地质现象,充分说明塘坝子、葛仙山等飞来峰是第四纪中更新世时“飞”来,压盖上去的。同时可见飞来峰与第四系之间是“冷接触”,找不到确切的断层证据。笔者等还用现有的区域地质调查资料及新的地质成果,编制了1:10万更新世时的彭县至汶川的地质剖面图,并设想了冰雪层掩盖情况。那时岷江尚未剥蚀下切,按现在标高计的5000m处,即在光光山、太子城之上约1000m的“天”上。当时应在该处出露的石炭系-二叠系石灰岩,就是塘坝子、葛仙山飞来峰的根部。塘坝子、葛仙山就是从那里被冰川作用剪切、从母体分离的石灰岩,滑动、随冰川固体流,滑移到彭县来的。笔者还从理论上阐述了塘坝子、尖峰顶、天台山等如此巨大的山体,能被冰川作用拔起、挖掉、推走的原因和根据。从而解释了飞来峰“飞”行的过程。顺理成章,合乎自然,揭开了飞来峰之迷。 相似文献
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彭县地区飞来峰的特征及形成演化 总被引:6,自引:1,他引:6
石绍清 《成都理工学院学报》1994,21(3):8-13
彭县地区飞来峰根据其内部构造特征和力学成因可分为两类-推覆体和滑覆体。推覆体是挤压环境下的产物,它形成于晚三叠世末期的印支运动。滑覆体是拉张环境下重力滑动的产物,它形成于燕山-喜马拉雅期。推覆体是滑覆体的“母体”。 相似文献
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龙门山中段山前带构造变形历史与物理模拟 总被引:2,自引:0,他引:2
龙门山冲断构造带具有NE分带、EW分段的构造变形特征。龙门山构造带中段逆冲推覆带是以出露彭灌杂岩及其前缘发育飞来峰为典型特征,变形以倾向北西的紧闭倒转-同斜褶皱为主;推覆-滑覆带变形强烈,发育一系列叠瓦状逆冲断层及相关的褶皱,及一系列由泥盆系至下三叠统碳酸盐岩构成的飞来峰,地腹发育厚皮构造,以叠瓦冲断构造为主;而前陆坳陷变形较弱,地表主要为SE倾伏的单斜,地腹则发育断层相关褶皱。通过构造物理模拟认为:1)龙门山中段构造变形受力边界主应力与断裂走向间的锐夹角为70°;2)变形样式总体为双滑脱层所控制的分层滑脱垂向叠加构造组合;3)构造变形过程具有3个阶段,早期须家河组沉积之后产生的滑脱断层垂向叠加,中期在遂宁组沉积期间和晚期在蓬莱镇组沉积期间及其后,发生滑脱断层垂向叠加,且控制沉积。 相似文献
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Desmond F. Lascelles 《Australian Journal of Earth Sciences》2013,60(1-2):161-165
Two inliers with a total outcrop length of 3000 m and a maximum width of 200 m, consisting of a sedimentary klippe (olistolith) and an olistostrome (both composed of banded iron‐formation and shale belonging to the Hamersley Group) occur within the Mininer Turbidite Member of the Wyloo Group, south of Paraburdoo, W.A., 2500 m from the top of the Hamersley Group proper. The olistostrome is a typical debris slide produced by slumping of unconsolidated material. The klippe was rafted into position as a solid block by a turbidity current. The pattern of mineralisation within the banded iron‐formation part of the klippe, which is identified as being from the Brockman Iron Formation, together with evidence from the basal conglomerate of the Wyloo Group, shows that the formation of the Hamersley iron ore deposits commenced prior to the deposition of the Wyloo Group sediments. 相似文献
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Michael A. Cosca Johannes C. Hunziker Sylvain Huon Henri Masson 《Contributions to Mineralogy and Petrology》1992,112(4):439-449
A combined 40Ar/39Ar, K/Ar, Rb/Sr and stable isotope study has been made of white micas from the Gummfluh klippe (Briançonnais domain of the Préalpes), Switzerland. The klippe consists mainly of Mesozoic to early Tertiary carbonate rocks metamorphosed from anchizonal to epizonal conditions. At the base of the klippe is a 10–50 m thick, ductilely deformed marble mylonite containing deformed authigenic quartz segregations. Stable isotope measurements of the coexisting calcite (18OSMOW=24.5) and quartz (18OSMOW=28.4) from the mylonite indicate relatively low temperatures (<300°C) during mylonitization. Analyses of white mica separates of varying size fractions from the mylonitic rocks by K/Ar and Rb/Sr techniques yield ages between 57 and 103 Ma. This variation is correlated with two parameters, the size of the mineral fraction, and the proportion of 2M1 (more phengitic) to 1M (more muscovitic) polytype in the sample. The K/Ar and Rb/Sr ages are generally younger in the smaller size fractions, which also containless 2M1 phengite. High precision 40Ar/39Ar age spectra from different size fractions of these micas record three distinct components, a small Hercynian component (ca. 200–300 Ma), a significant Eoalpine component (64–80 Ma) forming 40Ar/39Ar age plateaus, and a very minor Tertiary component (ca. 20–40 Ma). Characterization of the samples by SEM indicates the presence of two white mica populations, a coarser grained, deformed, detrital mica that probably corresponds to the 2M1 phengite and a finer grained neoformed 1M mica. Collectively these observations suggest that the Gummfluh samples contain a mixture of detrital phengites of Hercynian age together with neocrystallized muscovites grown during the late Eoalpine metamorphic event followed by minor argon loss during the Tertiary. The main geologic episode recorded in the 40Ar/39Ar age spectra of white micas in the mylonite is of Late Cretaceous/Early Tertiary age (64–80 Ma), representing the first reliable Eoalpine ages ever to be reported from the Préalpes. Contrary to tectonic models, the marble mylonite at the base of the Gummfluh klippe appears to be a Cretaceous thrust plane and not the thrust surface formed during transport of the klippe into its present position from the Penninic Alps during the Tertiary. The late Cretaceous thrust developed during marine sedimentation at a depth of 800 m below the seafloor at temperatures of 280°C, facilitated by warm fluids along the tectonic discontinuity. 相似文献
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A.P. Tewari 《Tectonophysics》1981,73(4):285-294
To the south of the Great Himalaya Range in Kashmir, a group of metasedimentary rocks with altered ultrabasic rocks occur physically over the migmatitic complex, as a klippe. The best exposure of it is met with in the Kudi nala, west of Sumjam, where lensoid outcrops of basic and ultramafic rocks, comprising actinolite—tremolite rock intruded by garnetiferous amphibolite occur within the marble, calc-gneiss and graphitic schist-gneiss. These rocks occur at an altitude of 5000–5500 m and the underlying rocks comprise gneiss, migmatite, schist, etc.The klippe of the metasedimentaries with the basic and ultrabasic suite of rocks, shows a synclinal disposition with a sheared northern contact. The southern contact of this klippe is also sheared and a tectonic “melange” zone is exposed in certain outcrops. This unusual geological set up, along with the absence of a deep-seated fault in the area of investigation, had led the author to believe that this suite of metasedimentaries has no stratigraphic relation with the underlying rocks which they override. These are very much akin to some of the rock suites of the Indus ophiolitic zone outcropping far in the north, particularly those of the Suru valley (Kargil tehsil) and they appear to have been transported during post-Cretaceous times as a thrust mass. This is the first record of an exotic thrust nappe in the Kashmir Himalaya to the south of the Great Himalaya Range. 相似文献