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Musa Alpaslan Taner Eki&#x;ci&#x; Nazmi&#x; Otlu Durmu Boztug Abi&#x;di&#x;n Temel 《Geological Journal》2005,40(2):193-214
The Miocene Karamağara volcanics (KMV) crop out in the Saraykent region (Yozgat) of Central Anatolia. The KMV include four principal magmatic components based on their petrography and compositional features: basaltic andesites (KMB); enclaves (KME); andesites (KMA); and dacites (KMD). Rounded and ellipsoidal enclaves occur in the andesites, ranging in diameter from a few millimetres to ten centimetres. A non‐cognate origin for the enclaves is suggested due to their mineralogical dissimilarity to the enclosing andesites. The enclaves range in composition from basaltic andesite to andesite. Major and trace element data and primitive mantle‐normalized rare‐earth element (REE) patterns of the KMV exhibit the effects of fractional crystallization on the evolution of the KME which are the product of mantle‐derived magma. The KMA contain a wide variety of phenocrysts, including plagioclase, clinopyroxene, orthopyroxene, hornblende and opaque minerals. Comparison of textures indicates that many of the hornblende phenocrysts within the KMA were derived from basaltic andesites (KMB) and are not primary crystallization products of the KMA. Evidence of disequilibrium in the hybrid andesite includes the presence of reacted hornblendes, clinopyroxene mantled by orthopyroxene and vice versa, and sieve‐texture and inclusion zones within plagioclase. The KMV exhibit a complex history, including fractional crystallization, magma mixing and mingling processes between mantle and crust‐derived melts. Textural and geochemical characteristics of the enclaves and their hosts require that mantle‐derived basic magma intruded the deep continental crust followed by fractional crystallization and generation of silicic melts from the continental material. Hybridization between basic and silicic melts subsequently occurred in a shallow magma chamber. Modelling of major element geochemistry suggests that the hybrid andesite represents a 62:38 mix of dacite and basaltic andesite. The implication of this process is that calc‐alkaline intermediate volcanic rocks in the Saraykent region represent hybrids resulting from mixing between basic magma derived from the mantle and silicic magma derived from the continental crust. Copyright © 2005 John Wiley & Sons, Ltd. 相似文献
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用传统方法拟合平稳河流的水位流量关系,往往精度不高,与实际测量不能很好的重合.对于局部线性的水位流量关系,用系统辨识理论对其进行建模,利用最小二乘法,拟合精度明显提高. 相似文献
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本文采用阿拉伯糖抗性正向突变试验（ara试验）并辅以鼠伤寒沙门氏菌组氨酸营养缺陷回复突变试验（Ames试验）对太湖梅梁湾冬季表层水样品致突变性进行分析研究，ara试验结果表明9个点样品中有5个（主要为入湖河口及近岸样品）表现显著的直接致突变性，加入哺乳动物来源的代谢活化系统S9后，结果仍呈现同样的趋势，A-mes试验在增加两倍半上样剂量的条件下表现出与ara试验大体一致的检出率，在本研究中，ara试验对于成分复杂的环境样品表现更高的检出灵敏度，表明ara试验作为首选方法来检测环境中复杂化学物基因毒性方面有良好前景。 相似文献
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井孔水位记震能力变化与近大地震关系研究 总被引：7，自引：0，他引：7
通过对云南省及邻近地区7级大震,震前群井水位记震能力变化的研究及异常、预报指标检验,表明震前记震能力减弱或消失与近大地震有关。其异常特征表现为形态相似、时间同步、幅度明显等特点。井孔水位记震能力变化可能是地下水中期预报地震的一种新方法。 相似文献
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宽级配砾质土应力路径试验研究 总被引：1，自引：0，他引：1
对某土石坝工程的宽级配砾质土进行了三轴等应力比应力路径试验,试验分别模拟了土石坝施工填筑期及蓄水期可能的应力路径,研究了宽级配砾质土在复杂应力状态下的应力应变特性。研究表明,砾质土心墙料在等主应力比和等主应力增量比应力路径作用下,应力应变表现出较好的线性关系;在竣工期,其平均主应力p（或剪应力q）与体应变ε_v及剪应变ε_s的曲线关系都为幂函数形式,ε_v—ε_1、ε_3—ε_1关系均可用线性函数来表示,而在蓄水期,各应力与应变之间的曲线关系则基本上都可以用线性关系来表示。本文研究明确了复杂应力路径下宽级配砾质土的应力应变关系,为建立宽级配砾质土的应力应变本构模型提供了一个重要线索。 相似文献
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