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61.
胶东福山—栖霞多金属成矿带是胶东重要的多金属矿产分布区,与成矿关系密切的主要为燕山期浅成—超浅成的酸性小型斑岩体。关于这些成矿小型斑岩体的形成时代、成因机制及构造背景以及与金矿密切相关的郭家岭岩体之间的关系的研究目前仍存在薄弱之处。本文选择香夼岩体、羊虎山岩体,在进行系统的野外地质调查基础上,进行岩石学、岩石化学、年代学等方面研究。结果表明,香夼岩体、羊虎山岩体锆石LA- ICP- MS U- Pb加权平均年龄分别为127. 9±0. 6 Ma、125. 6±0. 8 Ma,属于早白垩世。小型斑岩体SiO2含量为62. 28%~68. 59%,全碱含量为5. 50%~9. 30%,里特曼指数为1. 33~3. 38,Al2O3含量为13. 52%~14. 97%,P2O5含量为0. 06%~0. 14%,TiO2含量为0. 18%~0. 6%,Mg#介于30. 35~56. 70;轻稀土相对富集,具不明显的Eu负异常;富集大离子亲石元素Rb,亏损高场强元素Nb、Ta。岩石类型属于I型花岗岩,同时具有高锶低钇(Adakitic)岩石特征。小型斑岩体与金矿关系密切的郭家岭岩体具有一致的成岩时代,相似的地球化学和Sr、Pb同位素比值,反映小型斑岩体应为郭家岭期岩浆的浅成相。该期岩浆的形成与扬子板块和华北板块的碰撞造山俯冲折返后拆沉伸展和太平洋板块俯冲挤压的双重构造背景有关。 相似文献
62.
利用采自黄河源区阿尼玛卿山的祁连圆柏(Juniperus prezewalskii)样芯,采用国际规范的树轮学研究方法对所有树轮样芯进行了精确定年。针对各样芯不同的生长趋势分别采用负指数函数、线性函数和样条函数拟合与树龄有关的树木生长趋势。对个别在样芯中存在缺失段或缺失年轮过多难以准确判定缺失位置的样芯,采用"搭桥"的方法建立完整序列,最后用ARSTAN软件计算合成树轮宽度年表,最长序列为1532a,在满足复本要求的基础上建立了长度为830a的树轮宽度年表,并对年表的基本统计特征进行了分析。初步的分析结果表明该年表的年轮指数与研究区夏季温度成显著负相关,并在此基础上重建了研究区过去830年来夏半年(4~9月)平均最高温的变化。重建序列包含有大量的高频变化信息,又有十分显著的低频变化趋势。研究区在重建时段内经历了3个较为显著的降温期,其中1820s~1900s的降温趋势不同于该时期全球平均温度的升高趋势。另外,分析表明在重建时段内升温期较短,但是升温幅度大于降温幅度,迅速升温可能导致研究区严重干旱事件的发生。 相似文献
63.
Keyan Fang Xiaohua Gou Fahu Chen Jinbao Li Rosanne D’Arrigo Edward Cook Tao Yang Nicole Davi 《Climate Dynamics》2010,35(4):577-585
We present a Palmer Drought Severity Index reconstruction (r = 0.61, P < 0.01) from 1440 to 2007 for the southeastern Tibetan Plateau, based on tree rings of the forest fir (Abies forrestii). Persistent decadal dry intervals were found in the 1440s–1460s, 1560s–1580s, 1700s, 1770s, 1810s, 1860s and 1980s, and
the extreme wet epochs were the 1480s–1490s, 1510s–1520s, 1590s, 1610s–1630s, 1720s–1730s, 1800s, 1830s, 1870s, 1930s, 1950s
and after the 1990s. Comparisons of our record with those identified in other moisture related reconstructions for nearby
regions showed that our reconstructed droughts were relatively consistent with those found in other regions of Indochina,
suggesting similar drought regimes. Spectral peaks of 2.3–5.5 years may be indicative of ENSO activity, as also suggested
by negative correlations with SSTs in the eastern equatorial and southeastern Pacific Ocean. Significant multidecadal spectral
peaks of 29.2–40.9 and 56.8–60.2 years were identified. As indicated by the spatial correlation patterns, the decadal-scale
variability may be linked to SST variations in the northern Pacific and Atlantic Oceans. 相似文献
64.
We present a composite tree-ring chronology from two sites of Qilian Juniper(Sabina przewalskii)in the northwestern Qilian Mountains(QM),Northwestern China.Precipitation in June was found to be the main limiting factor for tree-growth.The tree rings are also significantly and positively correlated with June precipitation over large areas of the northern Tibetan Plateau(TP).The authors thus consider that the tree- ring based drought reconstruction from 1803–2006 is representative of a large area drought hist... 相似文献
65.
Jinbao Li Edward R. Cook Rosanne D’arrigo Fahu Chen Xiaohua Gou 《Climate Dynamics》2009,32(7-8):1173-1186
Moisture variability across China and Mongolia (hereafter, CM) during 1951–2005 was investigated using the recently developed monthly Palmer Drought Severity Index (PDSI) dataset. In total there are 206 PDSI grid points across CM, based on a 2.5° × 2.5° gridding system. For CM as a whole a significant decreasing trend in mean moisture availability was observed during 1951–2005, but with strong decadal (17.1-year) and interannual (5.0-year, 3.2-year, 2.4–2.8 year) variations. The areas affected by moderate and severe moisture deficit over CM have increased significantly since the mid-1950s. In contrast, there is a significant decreasing trend for areas affected by moderate wetness since the mid-1950s, and no significant trend was found for the areas affected by severe wetness. Ten moisture-related spatial patterns were objectively defined for CM using rotated Empirical Orthogonal Function (REOF) analysis. These patterns are related to distinct geographical areas and are associated with distinct temporal variations. Four of these patterns, in Northeast China (NE), North China (NC), Central China (CC), and East China (EC), generally demonstrate a significant decreasing trend in moisture availability. Two patterns located in western areas of Northwest China (NW) and the Tibetan Plateau (TP) show a significant moisture increase, while four patterns in Mongolia (MN), far western China (FW), South China (SC), and Southwest China (SW) do not have significant moisture trends during 1951–2005. Based on REOF results we propose that CM should be divided into ten coherent moisture divisions. Moisture variations within each division are generally coherent, but may show either similar or contrasting covariability with adjacent divisions. 相似文献
66.
满洲里南部白音高老组流纹岩锆石U-Pb定年及岩石成因 总被引:12,自引:3,他引:9
满洲里南部白音高老组火山岩主要由流纹岩组成,含少量珍珠岩和流纹质凝灰岩。LA-ICPMS锆石U-Pb定年结果显示,流纹岩形成于141~139Ma的早白垩世早期。岩石地球化学研究表明,火山岩具有高硅富碱、贫钙镁和高FeOT/MgO比值的特征; 稀土丰度总量较高(∑REE介于103×10-6~488×10-6),轻重稀土分馏明显[(La/ Yb)N=4.12~30.94)],Eu负异常显著(δEu=0.12~0.46); 微量元素以富集Rb、Th、U、K,强烈亏损Ba、Sr、P、Ti,中等亏损Nb、Ta和高Ga/Al值为特征,与A-型花岗岩特征相似。锆石176Hf/177Hf比值介于0.282785~0.282970之间,εHf(t)值均为正值,介于3.78~9.98之间。流纹岩岩浆来源于斜长石稳定区玄武质下地壳物质的部分熔融,形成于非造山板内伸展构造环境。 相似文献
67.
68.
下第三系名山组广泛分布于雅安地区,地层出露良好。本文简要介绍雅安国光山背斜东西两翼新测的地层剖面,将名山组(包括芦山组)划分成4段(砂岩粉砂岩段、粉砂岩泥岩泥灰岩段、泥岩粉砂岩段、泥岩段),并将芦山组归于名山组上部(Ⅳ段),从而取消该名称,综述了岩石组合特征、沉积环境,进行了生物地层和年代地层划分。 相似文献
69.
70.
改革开放以来广东省利用外资的时空差异特征 总被引:35,自引:3,他引:35
本文阐述了改革开放以来广东省利用外资的时空差异特征,结合国际内国政治经济形势将广东省利用外资的过程划分为5个阶段,并分析各阶段的主要特点,借助于定量分析方法考察外资在广东的地域分布特征及其形成原因,研究表明,改革开放以来广东省利用外资的不稳定增长过程和明显地域差异是省内各区投资环境的地域差异和国家外资政策综合作用的结果。最后,对广东省的经济发展和利用外资工作提出了建议。 相似文献