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991.
北祁连蛇绿岩的特征、形成环境及其构造意义 总被引:58,自引:1,他引:58
文中总结了北祁连蛇绿岩的特征,指出北祁连蛇绿岩大多具有MORB的性质,有玻安岩产出,形成在弧后和岛弧环境。北祁连蛇绿岩大多侵位在岛弧增生楔或活动陆缘地体之上,蛇绿岩属于科迪勒拉型,早古生代的北祁连造山带属于科迪勒拉型造山带。部分蛇绿岩之上整合产出一套沉积-火山岩系,称为蛇绿岩的上覆岩系。指出蛇绿岩及其上覆岩系的枕状熔岩分别来自不同的源区,具有不同的构造意义。还讨论了北祁连早古生代板块构造格局,认为北祁连洋盆属于古亚洲洋的一部分,可能曾经是一个较大规模的洋盆。献中通常把它当成增生或俯冲杂岩带的一部分来看待〔13,16-17〕;大岔大坂蛇绿岩带,其向两侧的延伸情况不清楚;九个泉(或塔墩沟)蛇绿岩带,向东可连到景泰县老虎山蛇绿岩,有人认为,向西可与榆树沟蛇绿岩相连〔20〕。早先认为,北祁连存在新元古代、中寒武和早-中奥陶世三个时代的蛇绿岩〔2,11〕,经过多年研究,目前大多数同意蛇绿岩主要是晚寒武-奥陶纪的〔13,16〕。图1北祁连早古生代蛇绿岩分布图1.前寒武纪基底;2.俯冲杂岩带;3.蛇绿岩。图中数字:1.九个泉;2.大岔大坂;3.边马沟;4.玉石沟;5.小八宝;6.百经寺;7.老虎山;8.榆树沟山2北祁连几 相似文献
992.
北补连蛇绿岩的特征,形成环境及其构造意义 总被引:23,自引:4,他引:23
文中总结了北祁连蛇绿岩的特征,指出北祁连蛇绿岩大多具有MORB的性质,有玻安岩产生,形成在弧后和岛弧环境,北祁连蛇绿岩大多侵位在岛弧增生楔或活动陆缘地体之上,蛇绿岩属于科迪勒拉型,早古生代的北祁连造山带属于科迪勒拉型造山带,部分蛇绿岩之上整合产出一套沉积一火山岩系,称为蛇绿岩的上覆岩系,指出蛇绿岩及其上覆岩系的枕状熔岩分别来自不同的源区,具有不同的构造意义,还讨论了北祁连早古生代板块构造格局,认为 相似文献
993.
南疆塔里木河流域生态环境近期变化的成因解释 总被引:3,自引:3,他引:3
徐羹慧 《沙漠与绿洲气象(新疆气象)》2005,28(2):28-31
南疆塔里木河流域的生态环境已引起社会和科技界广泛注意。本文分析了该地区生态环境近期变化的6个主要特点,并用自然和人文社会学观点解释了变化的成因,提出气候变化是该极干旱区生态环境变化中最活跃的主要自然因素及其影响方式,但在人类主要活动地区盆地主体,人类活动对生态环境变化起着决定性的作用。 相似文献
994.
(40)~Ar/(39)~Ar chronology and geochemistry of high-K volcanic rocks in the Mangkang basin, Tibet 总被引:9,自引:0,他引:9
ZHANG Huihua HE Huaiyu WANG Jianghai & XIE Guanghong Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou China Institute of Geology Geophysics Chinese Academy of Sciences Beijing China College of Life Sciences Sun Yat-Sen University Guangzhou China 《中国科学D辑(英文版)》2005,48(1)
Our two newly obtained high-quality 40Ar/39Ar ages suggest that the high-K volcanic rocks of the Lawuxiang Formation in the Mangkang basin, Tibet were formed at 33.5±0.2 Ma. The tracing of elemental and Pb-Sr-Nd isotopic geochemistry indicates that they were derived from an EM2 enriched mantle in continental subduction caused by transpression. Their evidently negative anomalies in HFSEs such as Nb and Ta make clear that there is an input of continental material into the mantle source. The high-K rocks at 33.5±0.2 Ma in the Mangkang basin may temporally, spatially and compositionally compare with the early one of two-pulse high-K rocks in eastern Tibet distinguished by Wang J. H. et al., implying that they were formed in the same tectonic setting. 相似文献
995.
A precise monitoring of snow surface height in the region of Lambert Glacier basin-Amery Ice Shelf,East Antarctica 总被引:2,自引:0,他引:2
I.Allison 《中国科学D辑(英文版)》2005,48(1):100-111
The net surface snow accumulation on the Antarctic ice sheet is determined by a combination of precipitation, sublimation and wind redistribution. We present a one-year record of hourly snow-height measurements at LGB69 (70°50'S, 77°04'E, 1850 m a.s.l.). east side of Lambert Glacier basin (LGB), and 4 year record at G3 (70°53'S, 69°52'E, 84 m a.s.l.), Amery Ice Shelf (AIS). The measurements were made with ultrasonic sensors mounted on automatic weather stations installed at two sites. The snow accumulation at LGB69 is approximately 70 cm. Throughout the winter, between April and September, there was little change in surface snow height (SSH) at the two sites. The negative SSH change is due to densification at LGB69, and is due to both ablation and densification at G3. The strongest accumulation at two sites occurred during the period between October and March (accounting for 101.6% at LGB69), with four episodic increasing events occurring during 2002 for LGB69, and eight events during 1999-2002 for G 相似文献
996.
Impact of warmer climate on melt and evaporation for the rainfed, snowfed and glacierfed basins in the Himalayan region 总被引:9,自引:0,他引:9
The impact of warmer climate on melt and evaporation was studied for rainfed, snowfed and glacierfed basins located in the western Himalayan region. Hydrological processes were simulated under current climatic conditions using a conceptual hydrological model, which accounts for the rainfall–runoff, evaporation losses, snow and glacier melt. After simulations of daily observed streamflow (R2=0.90) for 6 years, the model was used to study the impact of warmer climate on melt and evaporation. Based on the future projected climatic scenarios in the study region, three temperature scenarios (T+1, T+2 and T+3 °C) were adopted for quantifying the effect of warmer climate. The comparison of the effect of warmer climate on different types of basins indicated that the increase in evaporation was the maximum for snowfed basins. For a T+2 °C scenario, the annual evaporation for the rainfed basins increased by about 12%, whereas for the snowfed basins it increased by about 24%. The high increase of the evaporation losses would reduce the runoff. It was found that under a warmer climate, melt was reduced from snowfed basins, but increased from glacierfed basins. For a T+2 °C scenario, annual melt was reduced by about 18% for the studied snowfed basin, while it increased by about 33% for the glacierfed basin. Thus, impact of warmer climate on the melt from the snowfed and glacierfed basins was opposite to each other. The study suggests that out of three types of basins, snowfed basins are more sensitive in terms of reduction in water availability due to a compound effect of increase in evaporation and decrease in melt. For a complex type of basin, the decrease in melt from seasonal snow may be counterbalanced by increase in melt from glaciers. However, on long-term basis, when the areal extent of glaciers will decrease due to higher melt rate, the water availability from the complex basins will be reduced. 相似文献
997.
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999.
应用航磁数据分维计算推断火成岩的分布 总被引:2,自引:0,他引:2
计算巴彦浩特盆地航磁异常的分维数, 对计算出的分维数绘制等值线图, 并根据分形特征对该地区的火成岩进行划分, 得到了以往直接对航磁异常图进行推断解释所不能得到的良好地质效果。最后讨论如何选取最佳窗口和最佳网格来计算分维数, 并对此提出了2个经验。 相似文献
1000.