Superposed deformation in the Helanshan Structural Belt: Implications for Mesozoic intracontinental deformation of the North China Plate
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文摘

Syn-folding deformation shows a two-stage Mesozoic compressive field in the HSB.

The first tectonic event is presented by NNE–SSW shortening in T3–J1.

The WNW–ESE shortening then led to the formation of the superposed folds in J3–K1.

The HSB experienced the two-phase contractional deformation in the Mesozoic.

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