*Akira Usui1, Anna Nagaoka2, Go-Ichiro Uramoto1, Masafumi MURAYAMA3
(1.Marine Core Research Center, Kochi University, 2.Graduate School of Science, Kochi University, 3.Fac. Agriculture and Marine Sciences, Kochi University)
Keywords:marine manganese deposit, manganese crust, microstratigraphy, Shima-Shima-gaku
We attempted to apply the method of Shima-Shima-gaku (lamina stratigraphy named by prof. S. Kawakami) on the secular variations in growth structure, chemical and mineralogical properties between the growth columns of the hydrogenetic ferromanganese deposit. The critera for describing each bands or zones based on the macroscopic (=physical) properties are not always consistant with chronological correlations or may not match with mineral/chemical composition. Our microscopic characterization using optical microscope, XRF mapping, XRD, acid-leach, micro-focus X-ray CT proved a possibility of separating local and regional sources of each mineral particle or element which is closely associated the environments of eposition.