| 台马岩体的锶氧同位素研究 |
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| 引用本文： | 方清浩,何令仪.台马岩体的锶氧同位素研究[J].桂林工学院学报,1986(4). |
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| 作者姓名： | 方清浩 何令仪 |
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| 作者单位： | 桂林冶金地质学院地质矿产勘查系
(方清浩)，桂林冶金地质学院地质矿产勘查系(何令仪) |
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| 摘 要： | 台马岩体的地质学岩石学特征和锶、氧同位素特征一致表明,岩体的形成时代为海西晚期—印支早期;紫苏辉石花岗斑岩岩浆属壳源重熔岩浆,并在上侵定位过程中发生过深部同化混染作用。
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| 关 键 词： | 花岗岩 锡同位素 氧同位素 地质时代 岩石成因 |
A STUDY ON THE STRONTIUM AND OXYGEN ISOTOPES OF TAIMA INTRUSION IN GUANGXI |
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| Fang Qinghao,He Lingyi.A STUDY ON THE STRONTIUM AND OXYGEN ISOTOPES OF TAIMA INTRUSION IN GUANGXI[J].Journal of Guilin University of Technology,1986(4). |
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| Authors: | Fang Qinghao He Lingyi |
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| Affiliation: | Department of Geology |
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| Abstract: | Geology, petrology and the strontium and oxygen isotopes of Taimaintrusion simultaneously show that the intrusion formed in Late Hercyni-an Early Indosinian period. The magma of the hypersthene granite-porphyrybelongs to the crustal remelting type. In the process of emplacing, themagma experienced deep assimilation and contamination. |
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| Keywords: | granite strontium isotope oxygen isotope the time of formation genesis of rock |
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