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With the exception s of the Okinawa and Ayu tJOughs, al l the So utheast Asian marginal seas have formed by processes other than back-arc ex tension. The Andaman Sea is an ideal example of a leaky transform system. The West Phi lipp ine Sea, Banda Sea, Celebes Sea and S ulu Sea bas ins all appear to be remnants of former oceans now trapped behind younger arc-trench systems. The last three may be interpreted to be related to the post-Early Triassic rifting of the northern continental margin ofdoi:10.7186/bgsm20198611 fatcat:hmz52ihalrf4vfn4zbjk2yos3y