赣南—粤北白垩纪火山岩的地球化学特征及其成因机制讨论
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A Discussion on the Origin and Geochemical Characteristics of Cretaceous Volcanic Sequences in South Jiangxi and North Guangdong
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    摘要:

    通过对赣南—粤北白垩纪火山岩地球化学特征研究,得出火山岩系形成于一种过渡性构造环境(介于强烈挤压与强烈伸展之间)。其中,基性火山岩形成于走滑相对伸展环境,岩浆源自较深部,具亏损地幔性质;酸性火山岩形成于走滑相对挤压环境,岩浆源自较浅部,以壳源组分为主。它们共同构成过渡性岩浆杂岩建造。

    Abstract:

    Through discussion and analysis of the geochemical characteristics of C re taceous volcanic rocks in south Jiangxi and north Guangdong,it is concluded th at volcanic rocks are formed in a transitional tectonic environment (between the highl y compressed and the highly extended). Basic volcanic rocks occur in a rela tively extensional environment.The magma comes from the depth with a depleted m antle nature.Acid volc anic rocks are formed in the relatively compressed environment.The magma comes f rom the shall ow parts and is dominatedby crustal compositions.Together they constitu te the intermediate magmatic complex formation.

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张树明,巫建华,周维勋,左跃明,李清龙.1999.赣南—粤北白垩纪火山岩的地球化学特征及其成因机制讨论[J].地质论评,45(7):712-716,[DOI].
Zhang Shuming, Wu Jianhua, Zhou Weixun, Zuo Yueming, Li Qinglong.1999. A Discussion on the Origin and Geochemical Characteristics of Cretaceous Volcanic Sequences in South Jiangxi and North Guangdong[J]. Geological Review,45(7):712-716.

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