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Ma 11 (2)

• Coherent formation
• early - late Pleistocene
• Correlation: Middle part of Ma 11

• Sedimentary facies: Marine
• Lithofacies: Clay

• Upper limit: Unconformity
• Lower limit: Unconformity

------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown

• Distribution: Underground of Osaka plain

• Hongo (2009) Jour. Geol. Soc. Japan, vol.115, no.2, pp.64-79 DOI