福建武平岩基岩石谱系单位划分

根据近几年来在１：５万区调中采用岩石谱系单位新理论、新方法填图的成果，以及岩石成分、结构构造特征、群居关系、侵入接触类型等，将过去１：２０万区调均划属燕山早期黑云母花岗岩及细粒花岗岩的武平岩体，解体为志留纪、晚三叠世、侏罗纪、白垩纪等不同时代深成岩体，划分出中（基）性、中酸性及酸性岩等岩石类型。圈定深成岩体４０个，独立侵入体１５个，共３３个单元，归并为６个超单元，５个独立单元。并认为志留纪侵入岩浆

Classification of Litholineage Units of Wuping Batholith in Fujian Province

Wuping batholith is locatd in the boundary of Fujian Province and Guangdong Province and in the famous Shanghang-Yunxian NW-trending and Zhenghe-Dapu NE-trending tectomagmative active belts. The batholith was only put under early Yanshanina biotite granite and fine granite in the 1: 200000 regional geological surveying. According to the results by the new theory and methods of litholineage unit mapping (1: 50000 scale) and to the composition, textures, structures, and intrusive contact of the rocks, the batholith can be divided into Silurian, Late Triassic, Jurassic and Cretaceous plutons and intermediate (basic ), intermediate-acid and acid rocky types. It is dismembered for 40 plutons, 15 independent intrusive bodies, and 33 units, and grouped under 5 superunits and 1 sequence and 5 independent units. It is considered that the magma of Silurian intrusive rocks is remelting type, the magma of Triassic-Jurassic intrusive rocks mainly a syntexis type and the magma of Cretaceous intrusive rocks syntexis and differentiated types. It is found out that Silurian-Jurassic masses are mainly in the initiative emplacement in a compressed environment, and the Late Cretaceous-Early Jurassic masses are in the passive emplacement in a tensile environment. The emplacement environments are a close relationship with the NE and NW-trending faults.