Basic types and geologic significances of “truncation and onlap” unconformities |
Dengfa HE |
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Fig. 6. Characteristic of unconformity formed under the migration of fault-sag in the Saertai area, Yabulai basin. Anj—Pre-Jurassic; J2q—Middle Jurassic Qingtujing Fm.; J2x1— 1st Member of Middle Jurassic Xinhe Fm.; J2x2—2nd Member of Middle Jurassic Xinhe Fm.; J3s—Upper Jurassic Shazaohe Fm.; K— Cretaceous; E—Eocene; Q—Quaternary. |