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作 者:王联魁[1] 王谦身[2] 徐文新[1] 陈根文[1] 张绍立[1]
机构地区:[1]中国科学院广州地球化学研究所,广州510640 [2]中国科学院地质与地理物理研究所,北京100029
出 处:《高校地质学报》2005年第3期358-363,共6页Geological Journal of China Universities
摘 要:根据花岗岩系列和类型编图,华南地区浅源南岭系列(系列I)花岗岩多产于中部和西部,深源长江系列(系列II)花岗岩主要分布在东部。诸广山型(Ⅰ1型)、大容山型(Ⅰ2型)和关帝庙型(Ⅰ3型)花岗岩的重点分布区,分别在中心腹地、西部和西北部湖南境内;宁芜型(Ⅱ1型)、德兴型(Ⅱ2型)和闽浙沿海型(Ⅱ3型)花岗岩的重点分布区,分别在长江中下游、中西与中东部深断裂带、东南沿海地区。花岗岩系列、类型的趋势面分析和莫霍面深度变化与上述花岗岩系列、类型分布特点对应得非常好,它们的等值线变化趋势几乎重合,相互间吻合一致,可以认为花岗岩的形成与地幔莫霍面的隆起与坳陷密切相关,地幔隆起区产出深源系列II花岗岩,其中Ⅱ1、Ⅱ3型花岗岩尤为典型;地幔坳陷区发育浅源系列I花岗岩,以Ⅰ2、Ⅰ3型花岗岩很显著。Based on the mapping of the granitic series and types, strontium isotopic trend surface analyses and isobaths of Moho surface, the deep-level sourced Yangtze series ( series Ⅱ ) granitoids are mainly distributed in the eastern part of South China. The shallow-level sourced Nanling series ( series I ) granitoids are mainly distributed in the central and western parts of South China. The Ningwu type ( type Ⅱ 1 ), Dexing type ( type Ⅱ 2 ) and Fujing-Zhejiang cosatal type ( type Ⅱ3 ) granitoids are distributed in the middle-western, central-eastern and southeastern coastal parts of South China, respectively. The Zhuguangshan type ( type I 1 ), Darongshan type ( type I 2 ) and Guangdimiao type (type I 3 ) granitoeds are distributed in the central, western and northwestern parts of South China, respectively. The generation of granitoids is in close relation with the uplift or depression of the mantle ( Moho surface). The deep-level sourced granitoids (series Ⅱ ) , especially Ⅱ1,Ⅱ 3 types mainly occur in the uplift areas of the mantle, and shallow-level sourced granitiods ( series I ), especially I 2, I 3 type granitoids, mainly occur in the depression areas of the mantle.
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