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作者:... Reza Moussavi-Harami , Asadollah Mahboubi , Hossein Mosaddegh
来源:[J].Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen(IF 0.923), 2019, Vol.291 (2), pp.171-195
摘要:The Lower Carboniferous carbonate shallow marine sediments of the Mobarak Formation (Alborz Zone, northern Iran) are interpreted as a deepening-shallowing cycle interpreted as recording changes in relative sea level which correspond to depositional sequences. The field observatio...
作者:Asadollah Mahboubi , Soroush Modabberi
来源:[J].Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen(IF 0.923), 2019, Vol.295 (1), pp.61-89
摘要:Four Lower Cretaceous sections in the southern Yazd Block were measured and studied tointerpret the palaeoenvironments, synsedimentary tectonics, and sequence stratigraphy. TheEarly Cretaceous sedimentary record of this block, consisting of the Sangestan, Taft,Abkuh, and Darreh Z...
作者:Asadollah Mahboubi , Hossein Vaziri-Moghaddam ...
来源:[J].Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen(IF 0.923), 2015, Vol.276 (1), pp.121-146
摘要:A high-resolution well data in the Gachsaran and Bibi-Hakimeh oilfields and outcrops from nearby Mish Anticline, in the SE Dezful Embayment and the Izeh Zone of the Zagros Basin were used in this study to investigate facies and depositional settings of the Asmari Formation (Oli-g...
作者:Asadollah Mahboubi , Markus Wilmsen
来源:[J].Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen(IF 0.923), 2014, Vol.271 (1), pp.21-48
摘要:The Lower Jurassic Ab-Haji Formation which is widespread across east-central Iran but best exposed on the Tabas Block consists of sandstones, siltstones and mudstones deposited in fluvio- deltaic and marginal marine settings. Provenance studies of this formation record the geodyn...
作者:... Markus Wilmsen , Asadollah Mahboubi , Reza Moussavi-Harami
来源:[J].Newsletters on Stratigraphy(IF 2.429), 2014, Vol.47 (1), pp.21-59
摘要:Studies of stratigraphic sections of Cambrian rocks exposed in the central and eastern Alborz Mountains and in the Tabas area indicate characters that demand a revision of the upper Lower Cambrian (Series 2 – Series 3 boundary interval) through lowermost Ordovician lithostra...

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