其大地构造环境为大陆裂谷带。
贝加尔裂谷带是全球典型的大陆裂谷带之一，新构造运动强烈。
With intense neotectonic movement, Baikal rift zone is one of the typical continental rift zones in the world.
在空间上有成带分布特点，主要分布在裂谷带和被动大陆边缘，与同生断裂密切相关。
These ore deposits displaying belteddistribution mainly occurred in rift and passive continental margins, related to the syndepositional fractures.
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