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西伯利亚地台的金矿床和金矿化与中生代的碱性杂岩有关(1941;等,1967)。由碱性岩组成的岩体是很不均一的,我们将其分为三个建造:钾系列的碱性辉长岩型,正常碱性系列的二长岩——正长岩型和钠系列的碱性花岗岩型(岩浆岩建造……1979)。与这些碱性侵入岩伴生的还有碱性火山岩类,与此同时还发育有中心型的钙性的环状火山——侵入岩。对于该区内所研究的岩石而言,它与已研究过的钠质系列的碱性岩相比,前者没有大量的稀有及稀土矿化,但却显示出金的地球化
The gold deposits and gold mineralization on the Siberia platform are associated with Mesozoic alkaline complexes (1941; et al., 1967). The rock mass composed of alkaline rocks is very heterogeneous, and we divide it into three structures: alkaline gabbro type for the potassium series, monetite-normal-syenite series and sodium series for the normal alkaline series Alkaline granite type (magmatic rock construction ... 1979). Associated with these alkaline intrusive rocks are alkaline volcanic rocks, along with a central calcareous ring volcano-intrusive rock. For the studied rocks in this area, the former is not extensively mineralized with rare earths and rare earths compared to the already studied sodium series of alkaline rocks, but shows the geochemistry of gold