The Burakovka layered pluton of basic and mafic rocks is the largest intrusive massif in the Baltic Province composed of Si-and Mg-rich boninite-like rocks. The pluton consists of two individual bodies, each having its own internal structure, and contacting each other in their apical parts, known as the Aganozero and Shalozero-Burakovka bodies. Both bodies have a similar rock sequence including five differentiated zones (upward): mafic rocks, pyroxenite, gabbro norite, pigeonite gabbro norite, and magnetite gabbro diorite (the latter found only in the Shalozero-Burakovka Body). Being generally similar to each other, these bodies differ notably in the styles of their cumulate stratigraphy and, to a lesser extent, in composition. The pluton is distinguished by the presence of markers-singular interlayers of high-temperature mafic cumulates emplaced in the sequence of lower-T formations. Their origin is believed to have been associated with the intrusion of fresh magma portions into the crystallizing magma chambers. The same mechanism is believed to have been responsible for a macrorhythmic pattern found in the southeastern portion of the Shalozero-Burakovka intrusive body. Using chemical and mineralogical data, it is shown that the bodies discussed were derived from similar high-Si and high-Mg magmas, except that the Aganozero Body was emplaced 50 million years later than the Shalozero-Burakovka intrusion: the former was dated (Sm-Nd isochron) 2372±22 Ma (ε Nd = −3.22 ± 0.13), and the latter, 2433±28 Ma (ε Nd = −3.14 ± 0.14). It is concluded that the Burakovka Pluton was a long-lived magma center which developed above a local mantle plume, the origin of which had been associated with the activity of a megaplume which had been responsible for the existence of the Baltic province throughout a period of 200 million years.

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The Mesozoic potassic magmatism of the Central Aldan (southeastern Siberian Platform) consists of volcanic and intrusive rocks of diverse composition, including highly potassic alkaline (leucitites, phonolites, lamproites, phologopite pyroxenites, shonkinites, feldspathoid syenites) and moderately alkaline (trachytes, gabbros, monzonites, syenites) rocks. They have a different level of alkalinity, as well as special petrochemistry and mineralogy. In addition, the distribution of incongruent elements in the rocks practically is identical: they are enriched in large-ion lithophile elements (LILE) and light rare-earth elements (LREE) and impoverished in high-field strength elements (HFSE) and Ti0 2 . The Sr-and Nd-isotopic ratios in the potassic rocks of the Central Aldan vary considerably. They have low values of e Nd (T) (-10.2 to -22.9) and (87S r /86Sr) 0 = 0.70480 to 0.70723; that is, they differ from Chondritic Uniform Reservoir (CHUR) values in the field of an enriched mantle source of enriched mantle I (EMI) type and ancient lower crust. The wide variations in trace-element ratios (Ce/Y, Zr/Nb, Ba/La), like the variations in e Nd and e Sr , indicate a heterogeneous mantle source.

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