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.
研究表明，本区火山活动应为大陆板块内部的裂谷环境，与消减带无关。 文中还总结了火山活动的时代、规模、顺序、碎屑锥特点。研究了绳状、渣状熔岩的典型剖面、形成条件及流动方向。
The authors synthesized geological, geophysical and geochemical data, and believe that the plate tectonic setting of the study area should belong to the rift valley within the continental plate.
塔里木地块在北部古亚洲大陆拼贴和南部古特提洋打开影响下形成盆地，从天山到吉黑形成一系列的裂谷带（C1—P1）。
The Tarim basin was formed under control of the continental contage of Tarim block in Paleo-Asia continent and the open of Paleo-Tethys ocean. And rifting belt was formed in Tienshan-Jihei(C1-P1);
塔里木地块在北部古亚洲大陆拼贴和南部古特提洋打开影响下形成盆地，从天山到吉黑形成一系列的裂谷带（C1—P1）。
The Tarim basin was formed under control of the continental contage of Tarim block in Paleo-Asia continent and the open of Paleo-Tethys ocean. And rifting belt was formed in Tienshan-Jihei(C1-P1);
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