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221.
蛇绿岩就位机制可以划分出4种: 1)碰撞仰冲型:被动大陆边缘或岛弧与洋壳碰撞时,俯冲到一定深度的硅铝质物质在浮力作用下折返,并上驮相对完整的大洋岩石圈残片到达地表; 2)增生底垫型:洋底、海沟沉积物及海底较高地形的上层物质从俯冲板块上刮削下来,持续底垫到上覆板块之下,使大洋岩石圈残片逐渐被动抬高; 3)俯冲剥离型:断裂发育相对密集的洋中脊和转换断层等大洋岩石圈薄弱带,在滑脱断层的作用下大洋岩石圈上部层位的物质被剥离,在俯冲作用的驱动下被抬升; 4)角流型:从俯冲板块上刮削下来的大洋岩石圈残片被带入狭窄型或宽阔型增生楔,以管道流的方式进入深部并遭受高压变质作用,由低密度物质裹挟带出并就位至增生楔浅部。变质底板可以限定蛇绿岩就位的开始时限,后就位沉积物可以确定蛇绿岩就位的结束时间。 相似文献
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224.
高分辨率地震勘探技术贯穿于野外采集、室内资料处理和解释各个环节。文章从三维地震资料处理角度出发,探讨高分辨率、高信噪比和高保真度处理的关键技术措施,即波场净化处理,振幅、频率和相位补偿,叠前反褶积,静校正和动校正及叠后频谱整形。最后以实际资料说明经高分辨率处理后,频宽达到350Hz,给解释人员提供优质剖面,为分辨小间距薄煤层奠定基础。 相似文献
225.
226.
星叶石族矿物红外光谱研究 总被引:4,自引:0,他引:4
在新测定的星叶石晶体结构资料的基础上,对星叶石矿物进行了详细和红外光谱研究,对比了单斜及三斜星叶石的红光谱特征,并对星叶石中工外吸收振动的归属问题进行了讨论。 相似文献
227.
In order to investigate the distribution characteristics of stable carbon isotope ratios (δ
13C) in the desert plant Reaumuria soongorica, the δ
13C values of leaves were measured in 407 individuals of 21 populations. Soil physicochemical properties including soil water
content, soil total dissolved solids, soil total nitrogen, soil total phosphorus and soil organic content were also analyzed
in order to survey the major factors influencing δ
13C values on spatial variation. Leaves and soil samples were simultaneously collected from the ten major distribution areas
in Northwest China at altitudes from 394 m to 1 987 m above sea level, at latitudes from 36°10′N to 44°33′N, and at longitudes
from 81°43′E to 106°37′E. These ten areas include Shihezi, Baicheng, Yiwu areas in Xinjiang Uygur Autonomous Region; Anxi,
Zhangye, Baiyin, Lanzhou areas in Gansu Province; Shapotou, Yinchuan areas in Ningxia Hui Autonomous Region; and Alashan County
in Inner Mongolia Autonomous Region. The results show that the δ
13C value of R. soongorica ranges from −22.77‰ to −29.85‰ with an average of −26.52‰. Foliar d13C values in R. soongorica are not significantly correlated with altitude, latitude or longitude, and a spatial distribution trend of d13C values of
R. soongorica is not obvious on a large scale. However, when d13C values of two R. soongorica populations under the same climate conditions are compared, δ
13C values increase obviously from east to west and from north to south. As none of the soil total dissolved solids, soil total
nitrogen, soil total phosphorus, and soil organic content shows a uniform trend from east to west and from north to south,
we suppose that the small-scaled spatial distribution pattern of δ
13C values of R. soongorica is mainly controlled by the soil water content.
Translated from Quaternary Sciences, 2006, 26(6): 947–954 [译自: 第四纪研究] 相似文献
228.
The debris flow, which was triggered in the Wenjia Gully on August 13, 2010, is an extreme example of mass movement events, which occurred after the Wenchuan earthquake of May 12, 2008. This Earthquake triggered in the Wenjia Gully the second largest co-seismic landslide, which can be classified as a rockslide-debris avalanche. A lot of loose sediments was deposited in the basin. In the main so called Deposition Area II of this landslide, with a volume of 30?×?106?m3, flash floods can easily trigger debris flows because of the steep bottom slope and the relative small grain sizes of the sediments. The largest debris flow of August 13, 2010 destroyed the most downstream dam in the catchment during a heavy rain storm. The debris flow with a peak discharge of 1,530?m3/s and a total volume of 3.1?×?106?m3 caused the death of 7 persons, 5 persons were missing, 39 persons were injured and 479 houses buried. After three rainy seasons, only 16?% of the landslide-debris deposition was taken away by 5 large-scale debris flow events. Since the threshold for rainfall triggered debris flows in the Wenjia Gully and other catchments drastically decreased after the Wenchuan Earthquake, new catastrophic events are expected in the future during the rainy season. 相似文献
229.
Xisheng Xu William L. Griffin Xi Ma Suzanne Y. O’Reilly Zhenyu He Chengli Zhang 《Mineralogy and Petrology》2009,97(1-2):43-59
The "Taihua Group" is a collective term for a series of old terranes scattered along the southern margin of the North China Craton. The timing of formation and thermal overprinting of the Taihua Group have long been contentious, and its relationship with the Qinling orogenic belt has been unclear. In this study, new data from integrated in-situ U–Pb dating and Hf isotope analysis of zircons from an amphibolite (from the Xiong’ershan terrane) and a biotite gneiss (from the Lantian-Xiaoqinling terrane) indicate that the Upper Taihua Group formed during the Paleoproterozoic (2.3–2.5 Ga) and thus was originally part of the southern edge of North China Craton, detached during the Mesozoic Qinling orogeny and displaced about 100 km north from its original location. This suggests that the Taihua Group became part of the tectonic terrane associated with the Qinling orogeny and now forms part of the overthrust basement section of the Qinling belt. Before the Qinling orogeny, the Taihua Group was metamorphosed at 2.1 Ga. The initial Hf-isotope compositions of zircons, together with positive εNd(t) values for the whole-rocks, imply that the original magmas were derived from a juvenile source with some assimilation of an Archean crustal component. 相似文献
230.
一种自动绘制聚类分析谱系图的新算法 总被引:2,自引:0,他引:2
聚类分析是最常用的多元统计方法之一,其结果常用谱系图来表示,用计算机自动绘制谱系图时,过去常用的做法比较繁杂、新算法先将结果数据进行排序,再使用二叉树的方法,不算法直观,且速度加快。 相似文献