江苏东海片麻岩裂变径迹年龄和冷却历史     

杨刚  陈江峰  周泰禧  张巽  王世成 《矿物岩石地球化学通报》2001,20(4):306-308

本文测定了江苏东海科学超深钻选址地区地表和钻孔片麻岩样品的锆石和磷灰石的裂变径迹年龄。地表样品 97CK0 1的锆石裂变径迹年龄为 134± 11Ma ,磷灰石的裂变径迹年龄为 6 6 .8± 2 .5Ma。ZK2 30 4 85号样品磷灰石的裂变径迹年龄为 79.2± 2 .5Ma。由估计的锆石和磷灰石的裂变径迹封闭温度得到该地区从约2 2 5℃冷却到 10 0℃时的冷却速率为 (1.9± 0 .2 )℃ Ma ,在从约 10 0℃冷却到现在的冷却速率为 (1.0± 0 .1)℃ Ma。我们得到的结果不支持前人关于新生代加速冷却的结论 ,可能与地区的差异冷却有关。  相似文献   

冰川与气候关系的研究   总被引：5，自引：8，他引：5  

白重瑗 《冰川冻土》1989,11(4):287-297

  相似文献   

The Thermal History of the Huangmeijian Granite Intrusion in Anhiii and Its Relation to Mineralization: Isotopic Evidence     

Zheng Yongfei  Fu Bin  Gong Bing 《《地质学报》英文版》1996,9(2):168-180

Abstract Whole—rock Rb—Sr, zircon U—Pb and hornblende, biotite and K—feldspar K—Ar ages are used to reconstruct the cooling history of the Huangmeijian intrusion in the Anqing—Lujiang quartz—syenite belt in Anhui. Oxygen isotope geothermometry of mineral pairs demonstrates that diffusion is a dominant factor controlling the closure of isotopic systems. Assuming the cooling of the intrusion is synchronous with a dicrease in local geothermal gradients, an emplacement depth of about 8 km and the magma crystallization temperature of 800 ± 50°C are estimated. The Huangmeijian intrusion experienced a rapid cooling process and uplifted after its emplacement and crystallization at 133 Ma B.P. with a cooling rate of 34.5°C / Ma and an uplifting rate of 0.35 mm/ a. The intrusion was rising until it rested at a depth of 3 km at a temperature of 300 ± 50°C about 14 Ma later. Then the intrusion was in slow cooling and uplifting with a cooling rate of 4.4°C / Ma and an uplifting rate of 0.04 mm/ a. U—Pb dating of pitchblende is done for the hydrothermal uranium deposit formed in the contact zone of the Huangmeijian intrusion. The result shows that the mineralization age is close to the closing time of the K—Ar system in biotite. The fluid inclusion thermometry indicates that the mineralization temperature is in agreement with the closure temperature of the biotite K—Ar system. This suggests a close relationship between the slow cooling of the intrusion and the hydrothermal uranium mineralization process.  相似文献   

用超声速气流产生冰晶的试验及测定     

易仕明  酆大雄  陈汝珍  蒋耿旺 《气象学报》1994,52(3):368-373

在２ｍ３等温云室中进行了塑料小泡压爆及超声速气流在过冷雾中产生冰晶性能的试验，在－１℃到－１７℃温度范围内测试其产生冰晶效率。发现这两种方法均能在过冷雾中产生大量冰晶，直到－１℃。在－８℃时每升空气产生的冰晶为１０１１－１０１２量级。是一种经济有效的催化过冷云雾的方法，很有应用前景。  相似文献   

鲁西北西向断裂系晚中生代活动的几何学、运动学及年代学研究   总被引：3，自引：0，他引：3  

王先美 《地质学报》2008,82(9):1258-1273

鲁西隆起区发育有大量的北西向脆性断裂.依据野外断裂构造的几何学、运动学详细解析,认为北西向断裂系经历了早期的右行压剪、右行张剪,以及后期的左行压剪等不同性质的构造活动.由与北西向断裂活动相伴生的同期侵入岩体的 K-Ar测试结果分析,北西向断裂系在距今约160 Ma及距今130～110 Ma分别经历了右行压剪与右行张剪构造活动;通过分布在隆起区不同样品的磷灰石裂变径迹数据分析、冷却史反演,厘定鲁西地体在距今90～80 Ma存在一次区域性快速冷却构造事件,该构造事件与北西向断裂系的左行压剪构造活动相对应.  相似文献   

Late Mesozoic Thermotectonic Evolution of the Jueluotage Range,Eastern Xinjiang, Northwest China: Evidence from Apatite Fission Track Data   总被引：1，自引：0，他引：1  

ZHU Wenbin  WAN Jinglin  SHU Liangshu  ZHANG Zhiyong  SU Jinbao  SUN Yan  GUO Jichun  ZHANG Xueyun 《《地质学报》英文版》2008,82(2):348-357

Although many authors have emphasized the Cenozoic history of deformation, exhumation and cooling in the Tiaushan area related to the India-Asia collision, very little is known about the Mesozoic history of compression and uplift within the Tianshan. In order to obtain information about the Mesozoic exhumation history and processes of cooling in eastern Tianshan, fission track methods on apatite were used. Sampling was made in the Jueluotage Range. Three samples （Z001-Z003） were taken from granite in borehole ZK6301 of Yandong pluton; the ages range from 97.0 to 87.6 Ma that are much younger than the pluton age which was dated by U-Pb zircon at 334±2 Ma. Two samples in northern piedmont of the Jueluotage Range were collected from Jurassic strata in Dikaner （DK001） and Dananhu （D001） whose ages are 91.5 and 93.4 Ma respectively. The average apparent exhumation rate is 0.039 nun/a calculated by extrapolation on the basis of Yandong samples, indicating an extremely slow exhumation in the Jueluotage Range since the Late Cretaceous. Two Jurassic samples reached the maximum depths after deposition and experienced the maximum temperatures of ca. 105 and 108℃ until the late Early Cretaceous before a period of cooling and exhumation occurred at 114 and 106 Ma.  相似文献   

Permafrost Characteristics of the Qinghai-Tibet Plateau and Methods of Roadbed Construction of Railway     

NIU Fujun  XU Jian  LIN Zhanju  WU Qingbai  CHENG Guodong 《《地质学报》英文版》2008,82(5):949-958

Permafrost along the Qinghai-Tibet railway is featured by abundant ground ice and high ground temperature. Under the influence of climate warming and engineering activities, the permafrost is under degradation process. The main difficulty in railway roadbed construction is how to prevent thawing settlement caused by degradation of permafrost. Therefore the proactively cooling methods based on controlling solar radiation, heat conductivity and heat convection were adopted instead of the traditional passive methods, which is simply increasing thermal resistance. The cooling methods used in the Qinghai-Tibet railway construction include sunshine-shielding roadbeds, crushed rock based roadbeds, roadbeds with rock revetments, duct-ventilated roadbeds, thermosyphon installed roadbeds and land bridges. The field monitored data show that the cooling methods are effective in protecting the underlying permafrost, the permafrost table was uplifted under the embankments and therefore the roadbed stability was guaranteed.  相似文献   

全球变暖与变冷利弊分析     

刘秀铭  赵国永  李平原  吕镔  陈渠 《亚热带资源与环境学报》2013,(1):1-8

在联合国下属的政府间气候变化专门委员会（IPCC）的4次评估报告影响下,全球变暖达到前所未有家喻户晓的程度．各国人民似乎对“气候变暖”有谈虎色变的感觉．只要是灾难,不论水灾还是旱灾,不管是降温的雪灾还是高温的热浪,各国媒体均将这些灾害与“气候变暖”紧密联系起来,IPCC第四次报告也是如此．气候真的变暖了吗？真的那么严重变暖了吗？气候变暖真的给人类带来的只是可怕灾难而没有益处吗？水灾与旱灾是一对矛盾的2个方面,如何都能够由“全球变暖”一个因素所导致？地质记录表明,气候冷暖波动是地球气候变化一般形式,过去在人类能够影响大气二氧化碳含量以前,地球气候就是一直在不断地冷暖变化着的．驱动地球冷暖变化的主要因素是地球接收太阳辐射量的变化．不变的气候是短期的,是暂时的,而变化的气候却是长期和永恒的．持续了约550年变冷小冰期于1850年结束,随后进入暖期则是正常的自然过程．人类活动最大可能只是叠加了变暖的影响．本研究综合对比分析全球变暖和全球变冷2种气候变化所产生的一系列后果,认为全球变暖给人类带来结果是利大于弊．  相似文献   

Study on temperature field and settlement of thawing soil under static and dynamic loading     

LiYun Peng  JianKun Liu 《寒旱区科学》2013,5(5):0659-0666

A series of tests were conducted to analyze temperature field distribution and thawing settlement of a thawing soil under static and dynamic loading at various cooling and thawing temperatures. The res...  相似文献   

The prevalence of cooling cores in clusters of galaxies at z≈ 0.15–0.4     

F. E. Bauer  A. C. Fabian  J. S. Sanders  S. W. Allen  R. M. Johnstone 《Monthly notices of the Royal Astronomical Society》2005,359(4):1481-1490

We present a Chandra study of 38 X-ray-luminous clusters of galaxies in the ROSAT Brightest Cluster Sample (BCS) that lie at moderate redshifts  ( z ≈ 0.15–0.4)  . Based primarily on power ratios and temperature maps, we find that the majority of clusters at moderate redshift generally have smooth, relaxed morphologies with some evidence for mild substructure perhaps indicative of recent minor merger activity. Using spatially resolved spectral analyses, we find that cool cores appear still to be common at moderate redshift. At a radius of 50 kpc, we find that at least 55 per cent of the clusters in our sample exhibit signs of mild cooling  ( t _cool < 10 Gyr)  , while in the central bin at least 34 per cent demonstrate signs of strong cooling  ( t _cool < 2 Gyr)  . These percentages are nearly identical to those found for luminous, low-redshift clusters of galaxies, indicating that there appears to be little evolution in cluster cores since   z ≈ 0.4  and suggesting that heating and cooling mechanisms may already have stabilized by this epoch. Comparing the central cooling times to catalogues of central Hα emission in BCS clusters, we find a strong correspondence between the detection of Hα and central cooling time. We also confirm a strong correlation between the central cooling time and cluster power ratios, indicating that crude morphological measures can be used as a proxy for more rigorous analysis in the face of limited signal-to-noise ratio data. Finally, we find that the central temperatures for our sample typically drop by no more than a factor of ∼3–4 from the peak cluster temperatures, similar to those of many nearby clusters.  相似文献