As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

作为实例，我们重建了汤原断陷早第三纪中白垩系顶界三维古构造。

Then use antitone structural analysis method to recognize and reconstruct the primary tectonic structure and sedimentary feature of a basin in certain geological history.

要认识重建某个地质历盆地的原始构造格局沉积特征，就必须除去加的构造层构造变形，即反序构造分析法。

As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

作为实例，我们重建了汤原断陷早中期白垩系顶界维古构造。

Then use antitone structural analysis method to recognize and reconstruct the primary tectonic structure and sedimentary feature of a basin in certain geological history.

要认识重建某个地质历史时期盆地的原始构造格局沉积特征，就必须除去后期叠加的构造层构造变形，即反序构造分析法。

As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

作为实，我们重建了汤原断陷早第三白垩系顶界三维古构造。

Then use antitone structural analysis method to recognize and reconstruct the primary tectonic structure and sedimentary feature of a basin in certain geological history.

要认识重建某个地质历史时盆地的原始构造格局沉积特征，就必须除去后叠加的构造层构造变形，即反序构造分析法。

As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

作为实例，我们重建了汤原断陷早第三纪中期白垩系顶界三维古构造。

Then use antitone structural analysis method to recognize and reconstruct the primary tectonic structure and sedimentary feature of a basin in certain geological history.

要认识重建某个地质历史时期盆地的原始构造特征，就必须除去后期叠加的构造层构造变形，即反序构造分析法。

As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

作为实例，我们重建了汤原断陷早第三纪中期白垩系顶界三维古构。

Then use antitone structural analysis method to recognize and reconstruct the primary tectonic structure and sedimentary feature of a basin in certain geological history.

识重建某个地质历史时期盆地的原始构格局沉积特征，就必须除去后期叠加的构层构变，序构分析法。

As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

作为实例，我们重建了汤原断陷早第三纪中期白垩系顶界三维古构。

Then use antitone structural analysis method to recognize and reconstruct the primary tectonic structure and sedimentary feature of a basin in certain geological history.

要重建某个地质历史时期盆地的原始构格局沉积特征，就必须除去后期叠加的构层构，即反序构分析法。

As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

作为实例，我们重建了汤原断陷早第三纪中期白垩系顶界三维古构造。

Then use antitone structural analysis method to recognize and reconstruct the primary tectonic structure and sedimentary feature of a basin in certain geological history.

要认识重建某个地质历史时期盆地的原始构造格局沉积特征，就必须除去后期叠加的构造层构造变形，即反序构造分析法。

As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

作为实例，我们重建了汤原断陷早第三纪中期白垩系顶界三维古构造。

Then use antitone structural analysis method to recognize and reconstruct the primary tectonic structure and sedimentary feature of a basin in certain geological history.

重建某个地质历史时期盆地的原始构造格局沉积特征，就必须除去后期叠加的构造层构造，反序构造分析法。

As an example,the 3 D paleostructure of the boundary between Middle Eogene an...

作为实例，我们建了汤原断陷早第三纪中期白垩系顶界三维古。

Then use antitone structural analysis method to recognize and reconstruct the primary tectonic structure and sedimentary feature of a basin in certain geological history.

要认建某个地质历史时期盆地的原始格局沉积特征，就必须除去后期叠加的层形，即反序分析法。