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1.
为配合南京直立人生存时代和环境的研究,我们对南京汤山葫芦洞洞穴次生碳酸盐沉积物开展了年代学,同位素地球化学和显微岩相学等分析.6支石笋和5层钙板的TIMS铀系年龄测定结果表明,本区洞穴碳酸盐的发育时段几乎覆盖了0.5MaB.P.以来的地质时期。近30...  相似文献   

2.
本文根据灌阳县响水洞的成洞地质条件、生态环境以及洞穴的组成等,论述了洞穴的形成、发育过程。通过对响水洞1号石笋的铀系测年,碳氧同位素及沉积(间断)纹层分析,获得了距今44.0~3.1ka高分辨率古气候演变信息。反央44.0ka以来区内经历了严寒(晚大理冰期)、冰期后干冷和温热(间夹短暂的冷期)等气候变化,为确定响水洞的形成时代和环境提供了科学依据。  相似文献   

3.
用高精度、高灵敏度不平衡铀系热电离质谱(TIMS)法测定第卤纪地质年龄,并已在古气候、古环境、考古学以及近代活动火山作用的研究中取得了一系列重要成果。本文介绍了我们用MAT-262质谱仪对石笋、珊瑚进行测试并取得比较满意结果的情况。  相似文献   

4.
本文报道了用高精度热电离质谱(TIMS)法测定的贵州郑家洞AZJ-2号石笋的铀系年代。该石笋经历了三个速度不同的生长阶段,顶部90cm及底部21cm生长迅速,TIMS铀系法高分辨率年代结果仍不足以给出其确切的生长速率。精确建立碳氧同位素演化时间坐标的困难,应是从新生碳酸盐提取古气候演变信息的重要制约因素之一。AZJ-2的生长起止年代为距今14.7 ̄13.8万年,贵州在此期间可能处于温暖湿润的气候条  相似文献   

5.
热电离质谱(TIMS)U-Th年龄测定及其应用研究初探   总被引:6,自引:1,他引:6  
尝试了用热电离质谱方法测定南海第四纪珊瑚的U-Th年龄,并利用国家铀系年龄标准物质GBW04413来监测分析结果的合理性。结果显示,GBW04413的TIMS年龄与作为推荐值的α记数方法测定结果一致,反映出其可靠性;而年龄在1ka左右的珊瑚样品的TIMS年龄与14C年龄一致,>5ka样品的TIMS年龄老于14C年龄,体现两种方法的系统差别  相似文献   

6.
研究冰量较大时期千年尺度事件的区域响应和结构特征有助于进一步理解和验证千年尺度事件的驱动机制。基于湖北永兴洞一支石笋的5个高精度230Th年龄和323个氧同位素数据,重建了Dansgaard-Oeschger(DO)18事件发生时高分辨率的东亚水文循环变化的过程和特征。结合同一洞穴另两支石笋记录,发现永兴洞石笋δ18O在~64.7 ka迅速负偏1.5‰,指示在MIS4阶段东亚季风区确实发生了持续时间较短的DO18事件。石笋δ18O结果精确标定了DO18事件的结束时间为~63.0 ka,结束过程呈现出5个百年尺度的季风增强振荡。在形态特征上,不同于格陵兰冰芯DO18事件的快速开始和快速结束(~60 a)的对称变化,季风区DO18事件呈现出快速增强但缓慢结束(持续达1500 a)的显著不对称特征。但是,石笋δ18O与北大西洋温盐环流(AMOC)变化在形态特征和持续时间上高度一致,暗示了AMOC对东亚季风区DO事件的重要调控作用。DO18事件时东亚季风与北大西洋气候的不同结构特征可归于高低纬气候系统对AMOC响应方式的差异。石笋δ18O功率谱结果呈现出208 a、150 a、52 a和14~12 a的变化周期,分别接近于太阳活动的207 a、149 a、57 a和11 a周期,说明在冰量较大的MIS4阶段太阳活动仍控制着东亚季风短尺度的波动。  相似文献   

7.
石笋的ESR和 U系年龄及古气候研究   总被引:4,自引:0,他引:4       下载免费PDF全文
王兆荣  金嗣照 《地球科学》1995,20(6):677-681
对北京周口店第四地点洞穴的石笋进行了ESR测定,用封闭平衡模式计算了它们的ESR年龄,并与U系年龄地对比,它们的平均年龄十分一致,测定了石笋的氧和碳同位素,获得了北京地区(1.5 ̄0.5)×10^5a间古气候变化的信息。  相似文献   

8.
本文结合浮游有孔虫氧同位素地层学和不平衡铀系测定沉积速率的方法来确立取自南沙海域的沉积物柱样(NS90-103)的时间坐标、根据连续取样获得的δ(18)O曲线可以将该柱划分为7个主要气候期次,底部(550cm)相当于氧同位素第7.4阶到第7.5阶之间,年龄约238ka;而根据不平衡铀系的过量(230)Th方法获得2.3cm/ka的沉积速率,计算出底部年龄为239ka;两个结果在误差范围内完全一致。  相似文献   

9.
洞穴石笋古温度研究的同位素地球化学方法   总被引:6,自引:3,他引:6  
应用同位素地球化学方法,并以现代溶岩水的δ ̄18O_w代替石笋生长时期原生包体水的δ ̄18O_w,根据O’Neil方程,计算了福建宁化天鹅洞内第四纪碳酸盐堆积物的古温度。结果表明,温度计算偏差在±0.5℃左右。在与全球深海氧同位素曲线对比后,指出该地区大约在210~18kaBP,武木亚间冰期的起始时间(氧同位素期3/4阶界限)估计在65kaBP。结果表明,福建宁化地区晚第四纪古气候环境没有形成冰川的条件,但明显受到全球气温变化的控制。  相似文献   

10.
中国第四纪孢粉数据库(CPD)和生物群区(Biome 6000)   总被引:21,自引:0,他引:21  
介绍了中国第四纪花粉数据库的建立、组织及数据收集、大型成果共享等原则及章程,并着重介绍了当前由IGBP所支持的用孢子花粉资料重建6kaBP及18kaBP生物群区(植被)的全球合作项目。到目前为止,利用中国第四纪花粉数据的原始数据及生物群区化方法已经完成中国现代表土花粉、6kaBP(中全新世)及18kaBP(20kaBP)(末次盛冰期)的生物群区模拟及重建,在文中展示了制图结果,并讨论了当时植被与现  相似文献   

11.
Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.  相似文献   

12.
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.  相似文献   

13.
Robert L. Linnen   《Lithos》2005,80(1-4):267-280
The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H2O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H2O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.  相似文献   

14.
15.
Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ1 roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003).  相似文献   

16.
正20141520 Bo Ying(Key Laboratory of Metallogeny and Mineral Assessment,MLR,Beijing 100037,China);Liu Chenglin Saline Spring Hydrochemical Characteristics and Indicators for Potassium Exploration in Southwestern and Northern Tarim Basin,Xinjiang(Acta Geoscientica Sinica,ISSN1006-3021,CN11-3474/P,34(5),2013,p.594-602,5 illus.,3 tables,28 refs.)  相似文献   

17.
正20141243Chen Ge(Hangzhou Research Institute of Petroleum Geology,PetroChina,Hangzhou 310023,China);Si Chunsong Study on Sedimentary Numerical Simulation Method of Fan Delta Sand Body(Journal of Geology,  相似文献   

18.
正20142599Chen Sanming(Guangxi Key Laboratory of Concealed Deposits Exploration,Guilin University of Technology,Guilin541004,China);He Yuzhou Block Model and Reserves Estimation of Panzhihua Iron Deposit Based on 3D Geological Modeling(Journal of Guilin University of Technology,ISSN1674-9057,CN45-1375/N,33(4),2013,p.610-615,9illus.,1table,15refs.)  相似文献   

19.
正20140594 Bai Daoyuan(Hunan Institute of Geology Survey,Changsha 410016,China);Zhong Xiang Faults in the Jingzhou Basin and Their Tectonic Settings(Geotectonica et Metallogenia,ISSN1001-1552,CN44-1595/P,37(2),2013,p.173-183,6illus.,59refs.)Key words:basin evolution,tectonic setting,South China In the Upper Paleozoic and Jurassic se-  相似文献   

20.
正20141912Cao Hui(State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)Gravitational Collapse and Folding during Orogenesis:A Comparative Study of FIA Trends and Fold Axial Plane Traces(Geology in China,ISSN1000-3657,CN11-1167/P,40(6),2013,p.1818-1828,9illus.,35refs.,with  相似文献   

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