摘要
Multiple stratigraphic division and correlation sequence has been improved in the Shaoguan-Lianping area of northern Guangdong through lithostratigraphic, biostratigraphic and chronostratigraphic research. The investigation find that Sihui-Wuchuan fault zone enter Meizhou area starting from Sihui-Qixing area, and connected to Yingde-Shixing fracture group, and composing of widely silicified rock belt. Dadongshan-Guidong composite body is subdivided into 17 lithological units, among which middle Jurassic-early Cretaceous biotite monzonite contains the highest W-Sn contents,which maybe the source for W-Sn polymetallic deposits.