Facies, depositional sequences, and biostratigraphy of the oligo-Miocene Asmari Formation in Marun oilfield, North Dezful embayment, Zagros Basin, SW Iran
S Avarjani, A Mahboubi, R Moussavi-Harami… - Palaeoworld, 2015 - Elsevier
Abstract The Asmari Formation in Marun oilfield (south-west Iran), is about 440 m-thick
marine carbonate succession with subordinate siliciclastic rocks, characterized by abundant
benthic foraminifera (perforate and imperforate). Foraminiferal biostratigraphy indicates that
this unit is Oligocene–Miocene in age. The distribution of benthic foraminifera and other
components have led to the recognition of three siliciclastic and ten carbonate facies that
were deposited in inner ramp (shoreline, tidal flat, restricted and open lagoon and shoal) …
marine carbonate succession with subordinate siliciclastic rocks, characterized by abundant
benthic foraminifera (perforate and imperforate). Foraminiferal biostratigraphy indicates that
this unit is Oligocene–Miocene in age. The distribution of benthic foraminifera and other
components have led to the recognition of three siliciclastic and ten carbonate facies that
were deposited in inner ramp (shoreline, tidal flat, restricted and open lagoon and shoal) …
以上显示的是最相近的搜索结果。 查看全部搜索结果