辽西中生代陆内底侵作用背景下形成的安山岩

邵济安 路凤香 李伍平. 辽西中生代陆内底侵作用背景下形成的安山岩[J]. 岩石学报, 2007, 23(4): 701-708.
引用本文: 邵济安 路凤香 李伍平. 辽西中生代陆内底侵作用背景下形成的安山岩[J]. 岩石学报, 2007, 23(4): 701-708.
Mesozoic intracontinental andesites formed by underplating in west Liaoning province[J]. Acta Petrologica Sinica, 2007, 23(4): 701-708.
Citation: Mesozoic intracontinental andesites formed by underplating in west Liaoning province[J]. Acta Petrologica Sinica, 2007, 23(4): 701-708.

辽西中生代陆内底侵作用背景下形成的安山岩

  • 基金项目:

    国家自然科学基金(编号40372103,40672039)和中国科学院矿产资源研究重点实验室资助项目.

Mesozoic intracontinental andesites formed by underplating in west Liaoning province

  • 本文选择了辽西地区中生代230Ma、190Ma、159Ma、123Ma、116Ma等不同时期的安山岩及其所含的辉石,通过岩石学、岩相学、地球化学和同位素的研究,发现它们同时具有壳源和幔源的特征,而且大多数单斜辉石记录了两种或多种熔体的相互作用.据此作者认为安山岩是壳幔岩浆混熔成因的,而如此长期的热演化与大陆内部伸展背景下的底侵作用有关.
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出版历程
修回日期:  2006-08-22
刊出日期:  2007-04-30

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