Chemical Evolution of High Temperature Silicic Magmas

9614322 Nekvasil海洋和大陆热点环境和大陆裂谷地区的碱性岩组似乎来自比更常见的拉斑玄武岩更深的深度。 因此，它们应包含有关地幔物理和化学条件以及导致热点形成和裂谷作用的过程的重要信息。 通过对澳大利亚西北部南德瓦尔火山碱性玄武岩（夏威夷岩）分馏过程中长石成分演化的实验测定，可以揭示这些过程的解释。 此外，其他实验将解决的反应机制，其中三元晶石调整压力和温度的变化。 在这些实验中使用的斜长晶石是在玄武岩演化研究中产生的合成的斜长晶石，以及来自拉勒米斜长岩杂岩的Sybille正长岩的均质天然三元斜长晶石。

9614322 Nekvasil Alkalic rock suites in oceanic and continental hot spot environments and regions of continental rifting appear to come from greater depths than the more common tholeiites. Hence, they should contain important information regarding the physical and chemical conditions in the mantle as well as the processes that lead to hot spot formation and rifting. Elucidation of these processes may be revealed by experimental determination of the compositional evolution of feldspars during fractionation of an alkalic basalt (hawaiite) from the Nandewar Volcano, N.S.W. Australia. Additionally, other experiments will address the reaction mechanisms by which ternary feldspars adjust to changes in pressure and temperature. The feldspars utilized in these experiments are synthetic ones produced in the basalt evolution studies as well as homogenized natural ternary feldspars from the Sybille syenite of the Laramie Anorthosite Complex.