Выпуск: 2 , Том: 23 , Год издания: 1982

Basic-ultrabasic assemblages of Northern Baikal area associated with the ophio-litic belt have different structure-geological position and correspond to the following formational types: ultrabasite, gabbro-anorthosite and gabbro-peridotite. These assemblages were formed during endogenic conditions of geosynclinal and postorogenic types.