Basic types and geologic significances of “truncation and onlap” unconformities
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Basic types and geologic significances of “truncation and onlap” unconformities |
| Dengfa HE |
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| Fig. 8. Sketch of north-south geological profile crossing Well KP11-1-1 in Kaiping Sag, Pearl River Mouth Basin. Tg—base of Cenozoic; T85—base of the Middle Member of the Lower Wenchang Fm.; T84—base of the Upper Member of the Wenchang Fm.; T83—base of the Upper Wenchang Fm.; T82—base of the Middle Member of the Upper Wenchang Fm.; T81—base of the Upper Member of the Upper Wenchang Fm.; T80—base of the Oligocene; T72—base of the Middle Member of the Lower Oligocene Enping Fm.; T71—base of the Upper Member of the Enping Fm.; T70—base of the Upper Oligocene Zhuhai Fm.; T60—base of the Lower Miocene Zhujiang Fm.; T50—base of the Upper Member of the Zhujiang Fm.; T40—base of the Middle Miocene Hanjiang Fm.; T35—base of the Upper Member of the Hanjiang Fm.; T32—base of the Upper Miocene Yuehai Fm. |
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