palaeomagnetio evidence for the rotation of seram, indonesia
upper triassio shale from central seram give a directon of magnetization (D = 82 ,1 =23) which ( assuming, as seems probable ,that it was acquired before folding ,and during a priod of reversed magnetization) indicates seam lay 12_+ 7 s latitude and has rotated antilokwise 98 since the late triassic .the wquivalent ( south) palaeomagnetic pole is at 8 n, 207 e
Ketersediaan
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Pusat Sumber Daya Mineral, Batubara dan Panas Bumi - Jln. Soekarno Hatta No. 444, Bandung, Jawa Barat
PMB LK 1973-1