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- W2091227416 abstract "The upper Proterozoic Dovirensky layered complex has a strike length of 26 km and a stratigraphic thickness of about 3.2 km. The intrusion was emplaced 739 ± 55 Ma in the Proterozoic Baikal‐Vitim volcano‐sedimentary belt which is located between the Archaean Aldan Shield and the Siberian Platform. The supracrustal sequence was deformed and metamorphosed in a low amphibolite facies before the intrusion. The complex, with northwest strike and subvertical dip, is composed of a 1100 m thick ultramafic basal part of dunite overlain by a 300 m thick sequence of troctolite which grades upwards to a 1.3 km thick layered sequence of troctolite and olivine gabbro. Diopside oikocrysts characterize the transition zone from dunite to troctolite, and plagioclase and diopside oikocrysts characterize the zone from troctolite to olivine gabbro. A massive gabbronorite intruded the uppermost part, and gabbronoritic veins and sills are encountered in the lower part of the complex. Thin layers of anorthosite occur in troctoli..." @default.
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- W2091227416 date "1992-07-01" @default.
- W2091227416 modified "2023-09-26" @default.
- W2091227416 title "PGE in the upper Proterozoic Dovirensky layered complex, North Baikal area, Siberia" @default.
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- W2091227416 doi "https://doi.org/10.1080/08120099208728027" @default.
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