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1、
Lateral aggradation of continental strata is widely developed, resulting in highly variable litholo - gies and lithofacies.
陆相地层侧向加积作用广泛发育, 导致岩性、岩相多变.
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Lateral aggradation of continental strata is widely developed, resulting in highly variable litholo - gies and lithofacies.
陆相地层侧向加积作用广泛发育, 导致岩性、岩相多变.
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