鲁西铜石岩体的锆石SHRIMP U-Pb年龄及其地质意义   总被引：15，自引：0，他引：15  

胡华斌  毛景文  刘敦一  牛树银  王涛  李永峰  石玉若 《地学前缘》2004,11(2):453-460

首次报道了鲁西地区铜石岩体的锆石SHRIMPU Pb年龄结果。通过对斑状细粒闪长岩中单颗粒锆石 1 8个样品点的分析 ,获得了两组谐和年龄数据 ,其中有 1 0个分析点的2 0 6Pb/ 2 3 8U年龄为 1 6 7.9～ 1 83Ma ,加权平均值为 (1 75 .7± 3.8)Ma ;另外 8个分析点的2 0 7Pb/ 2 0 6Pb年龄为 2 5 0 2～ 2 5 5 4Ma ,加权平均值为 (2 5 1 8± 1 1 )Ma。二长斑岩样品仅获得 2个2 0 7Pb/ 2 0 6Pb年龄数据 ,在 2 4 85～ 2 5 1 2Ma之间。(1 75 .7± 3.8)Ma指示了铜石岩体的结晶年龄为中侏罗世 ,(2 5 1 8± 1 1 )Ma代表了岩体侵位过程中捕获的新太古代五台期锆石的年龄。根据SHRIMPU Pb年龄结果 ,认为鲁西地区存在燕山早期构造岩浆热事件 ,与之有关的归来庄金矿也在此时期形成  相似文献   

Rock glaciers in the northern Japanese Alps: palaeoenvironmental implications since the Late Glacial     

Masafumi Aoyama 《第四纪科学杂志》2005,20(5):471-484

In order to determine the palaeoclimatic and palaeo‐permafrost conditions in the northern Japanese Alps in central Japan, the ages of rock glaciers were investigated by relative age dating techniques such as weathering‐rind thickness and Schmidt hammer measurements. The results of the relative age dating suggest that the formation of the investigated rock glaciers may have started during the early phase of the Late Glacial or around the onset of the Holocene. The lower limit of current discontinuous permafrost in the northern Japanese Alps, which is indicated by the terminus of the lowest active/inactive rock glacier, lies at 2530 m a.s.l., while that of discontinuous permafrost during the Late Glacial or early phase of the Holocene, which is indicated by the terminus of the lowest relict rock glacier, lies at 2220 m a.s.l. Therefore, the lower limit of discontinuous permafrost during these periods would have been at least about 300 m lower than that of the current discontinuous permafrost. Climatic and geomorphological conditions during the Late Glacial led to a change in the environment from a glacial environment to a periglacial (permafrost) environment in the current alpine zone of the northern Japanese Alps. A large number of cirques were deglaciated and several of them were occupied by active rock glaciers around the onset of the Holocene. Copyright © 2005 John Wiley & Sons, Ltd.  相似文献   

Timing of mineralization and deformation,Peak Au mine,Cobar, New South Wales∗     

C. Perkins  M. C. Hinman  J. L. Walshe 《Australian Journal of Earth Sciences》2013,60(5):509-522

The ⁴⁰Ar/³⁹Ar dating of alteration muscovite from the Peak Au mine in the Early Devonian Cobar Basin, New South Wales, has distinguished two major episodes of mineralization. Veined (Pb‐Zn‐Cu‐Au) mineralization was broadly synchronous with cleavage formation during the post‐inversion, shortening deformation of the basin sedimentary rocks, and replacive Ag‐Pb‐Zn mineralization significantly postdates the latter event. Veined base metals (Pb‐Zn‐Cu) and Au associated with silicification were coeval with three stages of cleavage formation (D₁, D₂ and D₃) after basin inversion. The Cu‐Au phase of mineralization at the Peak Au mine which was broadly contemporaneous with the culmination of the cleavage‐forming events (D₃) and with the local development of high‐strain zones occurred at 401.5 ± 1.0 Ma (⁴⁰Ar/³⁹Ar on muscovite). This date is essentially coeval with known fossil constraints on the age of basin formation, and indicates that basin inversion and deformation rapidly followed sedimentation. In contrast, replacive Ag‐Pb‐Zn mineralization occurred at 384.0 ± 1.4 Ma (⁴⁰Ar/³⁹Ar on muscovite) during an extended period of relaxation characterized by normal faulting (D₄) which followed the shortening deformation. This mineralization was associated with desilicification and chlorite‐muscovite replacement assemblages which cross‐cut the cleavages, and which may have been broadly contemporaneous with the deposition of part of the Mulga Downs Group which unconformably overlies the Cobar Supergroup. Rhyolite exposed in the core of the Peak Au mine largely contains inherited zircons that range in age from ～430–1500 Ma. A few euhedral zircons have an age of ～430 Ma and this is interpreted as a maximum date for the rock. Zircons from a syn‐D₃ chlorite‐muscovite replacement zone within the deposit have ²⁰⁶Pb/²³⁸U ages of ～410–650 Ma and are apparently inherited.  相似文献   

Precise 14C ages of the Vedde and Saksunarvatn ashes and the Younger Dryas boundaries from western Norway and their comparison with the Greenland Ice Core (GICC05) chronology     

ØYSTEIN S. LOHNE  JAN MANGERUD  HILARY H. BIRKS 《第四纪科学杂志》2013,28(5):490-500

  相似文献   

城市功能空间更新研究进展与新时期重点方向   总被引：1，自引：0，他引：1  

隋洪鑫  杨秀  徐姗  周道静 《热带地理》2020,40(6):1150-1160

文章首先基于西方城市更新发展历程，界定了城市功能更新的概念内涵，进而围绕城市功能更新背景与演替轨迹、城市功能更新类型与组织模式、城市更新空间模拟识别与评价、城市功能更新驱动机理与规划调控等国内外研究进展进行系统梳理，研究发现，城市功能更新趋势与经济社会发展水平、城市化所处阶段紧密相关，更新运作模式体现为政府、私有部门和社区等多元合作倾向，更新判定趋于多源数据融合辨识，更新策略的制定受政策调控力、经济驱动力、市场机制等多重因素叠加影响。基于此，伴随新时期中国城市发展转型调整，城市功能更新研究更加重视对更新实践的科学性认知、空间治理能力的精细化转向、治理理念的人本化回归，并主要聚焦城市功能更新理论体系与实操框架的构建、功能业态演替特征的精细考量、更新调控的因地施策等新时期研究热点。但既有研究主要从城市与区域宏观尺度上对单一功能类型的更新模式进行定性描述，对微观视阈下精细功能业态演替的多时相认知与客观评价仍显不足。为此，提出未来中国城市功能更新应重视加强微观空间尺度下功能业态更新模式的多维度量化解析研究；在研究方法上，应注重融入系统学研究思想及其综合方法。  相似文献   

风浪对海-气界面动量通量估计的影响   总被引：1，自引：0，他引：1  

赵栋梁  李明明  马昕 《中国海洋大学学报(自然科学版)》2008,38(6)

利用实验室和有代表性的外海观测数据综合分析表明,海面粗糙度对波龄的依赖性与是否将实验室和外海数据一起考虑有关,而风应力拖曳系数与此无关,且随波龄增大而减小.利用Toba-3/2指数律和风浪成长关系的分析表明,风应力拖曳系数为常数或随波龄的增大而增大,与上述结果定性上相矛盾,说明风浪对风应力拖曳系数影响问题需要进一步研究.  相似文献   

Plankton, from the last ice age to the year 3007     

Pielou  E. C. 《ICES Journal of Marine Science》2008,65(3):296-301

  相似文献   

北秦岭西段凤县地区草滩沟群龙王沟组酸性凝灰岩年代学、岩石地球化学特征及其构造意义     

陈国超  张亚峰  裴先治  李佐臣  季宪军  魏均启  莫嵘桓  王超 《地质学报》2019,93(8):1968-1984

草滩沟群龙王沟组在北秦岭西段广泛出露,对研究秦岭早古生代构造演化具有重要意义。LA- ICP- MS锆石U- Pb同位素定年结果显示草滩沟群龙王沟组酸性凝灰岩的结晶年龄为457. 4±3. 8Ma。草滩沟群龙王沟组酸性凝灰岩富硅（SiO 2 =64. 55%~73. 07%）和碱（Na 2 O+K 2 O=5. 35%~8. 11%）,低铝（Al 2 O 3 =13. 91%~16. 07%）;轻稀土元素富集,重稀土元素亏损,具Eu负异常（δEu=0. 34~0. 86）;富集Rb、Th等大离子亲石元素(LILE),亏损Nb、Ta、Ti等高场强元素(HFSE),具有较低的Nb/Ta比值和Mg # 值。以上显示,草滩沟群龙王沟组酸性凝灰岩具壳源特征,为地壳部分熔融结果。北秦岭造山带草滩沟群龙王沟组酸性凝灰岩和晚奥陶世—早志留世岩浆岩具弧岩浆岩特征,显示它们形成于俯冲环境。结合北秦岭造山带早古生代超高压变质带、岩浆岩分布以及草滩沟群沉积特征显示,早奥陶世北秦岭造山带还处于商丹洋的俯冲阶段。  相似文献   

甘肃窑街植物群的地质时代及古地理区系研究     

辛存林  王露菡  季健健  张亚梅  王晶菁 《地质学报》2019,93(2):302-316

本文对甘肃窑街组古植物群及古地理进行研究,共发现植物化石31属63种,以银杏类(36.5%)和真蕨类(22.2%)繁盛,松柏类(17.5%)和苏铁类(15.9%)占一定比例,楔叶类(6%)、不明位置的果与穗(1.9%)为特征。在此基础上结合植物群组成分子指示的时代特征,以及与国内外同期其它植物群的对比,认为窑街组植物群的地质时代为中侏罗世早中期(Aalenian-Bajocian)。利用聚类分析法对甘肃窑街及其余11个研究较为细致的中国北方中侏罗世植物群进行对比,探讨甘肃窑街古地理归属,并对中国北方中侏罗世植物区进行初步划分。利用分支生物地理分析法研究甘肃窑街植物群的亲缘关系,结果表明窑街中侏罗世植物群与内蒙古高头窑植物群关系较为亲近;讨论了甘肃窑街新发现的屈囊蕨属在中国的地理分布特征,发现其分布与中国北方中侏罗世的初步区划结果吻合。  相似文献   

辽西髫髻山组的形成时代及地球化学特征     

李斌  陈井胜  刘淼  杨帆  吴振  杜继宇 《地质论评》2019,65(Z1):63-64

正髫髻山组在辽西—冀北地区广泛分布,在辽西地区,主要分布在金岭寺—羊山盆地、北票盆地、凌源地区等。在辽西—冀北地区,髫髻山组与之上的土城子组常同时出露,两者的接触关系是平行不整合;底部整合压盖于海房沟组复成分砾岩之上。髫髻山组火山岩测年数据较多,但是测年数据差异较大,导致对髫髻山组的形成时代、背景等方面的认识不同。因此,本文对辽西朝阳地区的髫髻山组火山岩进行了锆石U-Pb测试及地球化学研究。  相似文献