The arc-trench system and the distr

The arc-trench system and the distribution of diorite in the Philippines is mentioned first. And three epochs of diorite intrusion during the Tertiary Era were differentiated. The Paleocene diorites are distributed in the innermost zone of the mobile belt covering the Mindoro-Visaya—northwest Mindanao area. The Eocene—Oligocene diorites are distributed along the eastem coast of Luzon ls. where a collision of microcontinent-island arc is assumed. The middle Miocene to the uppermost Miocene diorites are distributed along the present "two reversely fronting arcs".

Hasil (Bahasa Indonesia) 1:

Sistem arc-palung dan distribusi diorite di Filipina disebut pertama. Dan tiga zaman diorite intrusi selama Era tersier yang dibedakan. Diorites Paleosen didistribusikan di zona terdalam sabuk mobile meliputi Mindoro-Visaya — barat laut Mindanao daerah. Eosen — Oligocene diorites didistribusikan sepanjang eastem pantai Luzon ls. mana tabrakan microcontinent-pulau Arc diasumsikan. Pertengahan Miosen untuk diorites Miosen teratas didistribusikan sepanjang hadir "busur terbalik fronting dua".

Hasil (Bahasa Indonesia) 2:

Sistem busur-parit dan distribusi diorit di Filipina disebutkan pertama. Dan tiga zaman intrusi diorit selama Tersier Era dibedakan. Paleocene batuan diorit didistribusikan di zona terdalam dari sabuk ponsel meliputi wilayah Mindoro-Visaya-laut Mindanao. Eosen-Oligosen batuan diorit didistribusikan sepanjang pantai eastem dari ls Luzon. di mana tabrakan dari mikrokontinen-pulau busur diasumsikan. Miosen tengah ke batuan diorit Miosen teratas didistribusikan sepanjang hadir "dua busur terbalik sepertinya".