Comptes Rendus De L Academie Des Sciences Serie 2 Mecanique Physique Chimie Sciences De L Univers Sciences De La Terre, 1990
The Philippine Fault is a plio-pleistocene left lateral strike-slip fault. By considering geologi... more The Philippine Fault is a plio-pleistocene left lateral strike-slip fault. By considering geological and kinematic data, we propose an age of 2 to 4 Ma and a displacement rate of 2 to 3 cm/yr. The Philippine Fault originates from the flip of subduction from West to East along the Philippine Mobile Belt. It is assumed to be the result of the collision of Halmahera with the southern Philippine Mobile Belt
Abstract Two volcanic belts are presently juxtaposed on Mindanao Island in the southern Philippin... more Abstract Two volcanic belts are presently juxtaposed on Mindanao Island in the southern Philippines. Southward, the collision is still active in the Molucca Sea which is commonly regarded as a region of doubly verging subduction, plunging eastward below the ...
Comptes Rendus De L Academie Des Sciences Serie 2 Mecanique Physique Chimie Sciences De L Univers Sciences De La Terre, 1990
The Philippine Fault is a plio-pleistocene left lateral strike-slip fault. By considering geologi... more The Philippine Fault is a plio-pleistocene left lateral strike-slip fault. By considering geological and kinematic data, we propose an age of 2 to 4 Ma and a displacement rate of 2 to 3 cm/yr. The Philippine Fault originates from the flip of subduction from West to East along the Philippine Mobile Belt. It is assumed to be the result of the collision of Halmahera with the southern Philippine Mobile Belt
Abstract Two volcanic belts are presently juxtaposed on Mindanao Island in the southern Philippin... more Abstract Two volcanic belts are presently juxtaposed on Mindanao Island in the southern Philippines. Southward, the collision is still active in the Molucca Sea which is commonly regarded as a region of doubly verging subduction, plunging eastward below the ...
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