形成这样的地质环境条件主要是岩浆侵入作用导致上覆火山岩的褶皱构造、侵入体的岩穹构造及接触破碎带构造等。
The geologic environment was mostly resulted from the intrusion of magma which led to folding of the overlying volcanic series, the formation of the intrusive dome and the contact broken zone.
结合台马碎斑熔岩与周边火山岩、侵入岩、地层的关系，认为它是早—中三叠世中心裂隙式火山构造中央部位侵出的穹状岩脊。
Combined with the surrounding volcanic rocks, intrusive rocks and strata, the Taima rock body is considered as a dome of the central part of the central fissure type volcanic structure.
柴达木盆地北缘是重要的构造-岩浆活化带和内生矿产成矿带，现今大地构造性质属地穹列。
The north margin of Qaidam basin is a significant tectonic-magmatic activation belt and an endogenic metallogenic province. Its recent architectonic property is a geodome series.
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