Origin and episodic emplacement of the Manaslu Intrusive Complex
Origin and episodic emplacement of the Manaslu Intrusive Complex
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DOI：
10.1093/petroj/40.1.3
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发表时间：
1999
期刊：
影响因子：
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通讯作者：
T. Harrison;M. Grove;D. Kevin;K. McKeegan;C. Coath;O. Lovera;P. Lefort
中科院分区：
文献类型：
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作者：
T. Harrison;M. Grove;D. Kevin;K. McKeegan;C. Coath;O. Lovera;P. Lefort
减压以达到同样的结果似乎需要极端的马纳斯卢花岗岩是最多的研究十几个岩体的条件不允许现有的地质约束。构成了高喜马拉雅浅色花岗岩带马纳斯卢花岗岩与重要的喜马拉雅构造构造的推断关系激发了人们反复尝试确定其结晶年龄，但几个地球化学控制阻碍了这些地质年代学研究。独居石的Th-Pb离子微探针测年克服了这些局限性。我们有
decompression to achieve the same result appear to require extreme The Manaslu granite is the most studied of the dozen or so plutons conditions not permitted by available geological constraints. that make up the High Himalayan leucogranite belt. The inferred relationship of the Manaslu granite with important Himalayan tectonic structures has inspired repeated attempts to determine its crystallization age, but several geochemical controls have hampered these geochronological investigations. These limitations are circumvented by Th–Pb ion microprobe dating of monazite. We have