Most of the ore deposits are located in the ore-magmatic systems, which are spatially and genetically connected with the ring structures. Studying of the geology and all available map materials allows to detect the type and background of different signs of deposit mineralization and to develop the criteria for exploration of mineral deposits.
1. Solomin A.N. Geohimicheskie kriterii poiskov i prognozirovanija zolotorudnyh mestorozhdenij Central'nogo Aldana (Juzhnaja Jakutija). Avtoref. Kand. dis., 1988. – 19 s.
2. Solomin A.N. Rudno-magmaticheskie sistemy kristallicheskih shhitov. Materialy nauchnoj konferencii “Novye gorizonty v izuchenii processov magmo- i rudoobrazovanija”. – M.: IGEM RAN. – 2010. – S. 161–162.
3. Ugrjumov A.N. Opyt formacionnogo analiza zolotorudnyh dzhasperoidnyh mestorozhdenij pri krupnomasshtabnom prognoze i poiskah // Formacionnyj analiz i krupnomasshtabnyj prognoz rudnyh mestorozhdenij. – M. – 1987. – S. 70–77.
4. Maksimov E.P. Opyt formacionnogo analiza mezozojskih magmaticheskih obrazovanij Aldan-skogo shhita // Izv. ANSSSR. Ser .geol., 1975. – (4). – S. 16–32.
5. Kochetkov A.Ja. Mezozojskie rudno-magmaticheskie sistemy Aldanskogo shhita // Tezisy dokladov simpoziuma “Glubinnoe stroenie Tihogo okeana i ego kontinental'nogo obramlenija”. – Ch.Sh. Blagoveshhensk. – 1988. – S. 38–40.