معرفی رخساره های لرزه ای، رسوبات خلیج‌فارس در شمال جزیره قشم‏

Using high-resolution shallow seismic data, we have investigated the seismic facies in northern qeshm island waterways in east of persian ‎gulf. seismic data obtained with sub-bottom profiler and then interpreted by ise software. studies lead to recognizing 7 types seismic facies ‎on seismic data. these facies are detectable by amplitude, continuity, geometry, internal pattern and staking pattern from each other. results ‎show that seismic facies formed in two various environments condition. lower part facies have low amplitude with high lateral continuity ‎and sustainability; but upper seismic facies have various amplitude with low lateral continuity. these facies have deposited in five periods ‎that separate with erosional surfaces. changes of depositional environments and province region of sediment supply can be realize from ‎seismic facies. so, through deposition of lap-c and mac facies sediments have supplied from qeshm island; but, at the time of deposition ‎of lac and hac sediments interred from the north.‎