Publication: [628] The Ashigara Group, a regressive submarine fan-fan delta sequence in a Quaternary collision boundary, north of Izu peninsula, central Honshu, Japan




Documented Paleocurrents


# Continental Area Stratigraphic Level Total Records Period Latitude Longitude Tectonic Plate Deposition Environment Paleocurrent Type Lithology Formation
1 Indo-Australian Lower Pliocene 11 45124 35.61 139.02 Indo-Australian marine deep paleocurrent indicator not specified sandstone Ashigarn
2 Indo-Australian Lower Pliocene 11 45124 35.4 139.01 Indo-Australian marine deep paleocurrent indicator not specified sandstone Ashigarn
3 Indo-Australian Lower Pliocene 11 45124 35.3 139.05 Indo-Australian marine deep paleocurrent indicator not specified sandstone Ashigarn
4 Indo-Australian Lower Pliocene 11 45124 35.5 139.2 Indo-Australian marine deep paleocurrent indicator not specified sandstone Ashigarn
5 Indo-Australian Lower Pliocene 11 45124 35.3 139.1 Indo-Australian marine deep paleocurrent indicator not specified sandstone Ashigarn
6 Indo-Australian Lower Pliocene 11 45124 35.7 139.2 Indo-Australian marine deep paleocurrent indicator not specified sandstone Ashigarn
7 Indo-Australian Lower Pliocene 11 45124 35.55 139.03 Indo-Australian marine deep paleocurrent indicator not specified sandstone Ashigarn
8 Indo-Australian Lower Pliocene 11 45124 35.61 139.1 Indo-Australian marine deep paleocurrent indicator not specified sandstone Ashigarn
9 Indo-Australian Lower Pliocene 11 45124 35.63 139.01 Indo-Australian marine deep paleocurrent indicator not specified sandstone Ashigarn
10 Indo-Australian Lower Pliocene 11 45124 35.5 139.5 Indo-Australian marine deep paleocurrent indicator not specified sandstone Ashigarn
11 Indo-Australian Lower Pliocene 11 45124 35.2 139.01 Indo-Australian marine deep paleocurrent indicator not specified sandstone Ashigarn