北淮阳盆岭构造带是大别造山带的重要组成部分。
Beihuaiyang basin and range structural belt is an important part of Dabie orogenic belt.
豫西地区位于华北地台南缘华-熊地块区，具典型的盆岭构造特征。
The Western Henan, situated in the Hua-Xiong massif of the southern margin of the North China Platform, is of typical basin-range structure.
不少学者用变质核杂岩模式解释豫西后造山阶段的基底隆起和与之相伴的盆岭构造的构造格局。
Using metamorphic core complex (MCC) models, many geologists interpret the tectonic framework featuring the basement dome and the basin-and-range tectonics in western Henan in the postorogenic stage.
通过磷灰石裂变径迹热史模拟的方法，精确揭示了在新生代时期松辽盆地与大兴安岭的热构造史，并分析了它们的盆山耦合关系。
Thermal history simulation of Apatite Fission Track shows that the thermal structure history in Cenozoic and the relationship between Songliao Basin and Dahinganling Mountain.
通过磷灰石裂变径迹热史模拟的方法，精确揭示了在新生代时期松辽盆地与大兴安岭的热构造史，并分析了它们的盆山耦合关系。
Thermal history simulation of Apatite Fission Track shows that the thermal structure history in Cenozoic and the relationship between Songliao Basin and Dahinganling Mountain.
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