Arid
DOI10.1007/s00531-019-01778-8
Microfacies, biofacies, and depositional environments of the Bajocian-Bathonian Middle Dhruma carbonates, central Saudi Arabia
Ismanto, Aviandy W.1; Chan, Septriandi A.1; Babalola, Lamidi O.2; Kaminski, Michael A.1; Al-Ramadan, Khalid A.1; Abdullatif, Osman M.1
通讯作者Babalola, Lamidi O.
来源期刊INTERNATIONAL JOURNAL OF EARTH SCIENCES
ISSN1437-3254
EISSN1437-3262
出版年2019
卷号108期号:8页码:2577-2601
英文摘要Three cliff-forming outcrops of the Dhruma Formation representing the carbonate platform in the Hafirat Nisha district west of Riyadh, Saudi Arabia, were investigated to identify and understand the microfacies variability in a carbonate ramp setting. An integrated approach including detailed field investigations, petrographic, biofacies, and micropaleontological analyses was used to construct a model of the depositional environments of the investigated outcrop sections. The depositional model indicates that the identified lithofacies were predominantly deposited in outer ramp, middle ramp, inner ramp, and lagoonal settings. The presence of the benthic foraminifera Redmondoides lugeoni and Nautiloculina oolithica and the trace fossil Thalassinoides indicates deposition in shallow-water environments and the prevalence of warm climatic conditions during the Middle Jurassic. The occurrences of calcareous and agglutinated benthic foraminiferal species Pseudomarssonella maxima, Siphovalvulina variabilis, Timidonella sarda, N. oolithica, R. lugeoni, Praekurnubia crusei, Paleopfenderina salernitana, Haurania deserta, Siphovalvulina spp., Lenticulina sp., Textulariopsis sp., and Amijella amiji imply that our studied sections are situated within the Dm-2 to Dm-5 biozones (Bajocian to early Bathonian). This is also supported by the calcareous nannofossil assemblages that show a Bajocian to early Bathonian age. The depositional sequences indicate a shift in the depositional environment from low-energy lagoonal with intermittent shoal complexes in the D2 and D3 Units to predominantly shoal complex and open-marine settings in the D4 Unit, suggesting a seaward shift towards the top of the D4 Unit. The interpreted depositional settings are similar to those previously documented in the subsurface equivalent, Faridah reservoir. This indicates that the investigated D2-D4 Units outcrops are excellent analogues of the subsurface reservoir.
英文关键词Middle Jurassic Dhruma formation Saudi Arabia Microfacies Paleoenvironment
类型Article
语种英语
国家Saudi Arabia
收录类别SCI-E
WOS记录号WOS:000493756400001
WOS关键词SEQUENCE STRATIGRAPHY ; RAMP SUCCESSION ; FORAMINIFERA ; PLATFORM ; BIOSTRATIGRAPHY ; EVOLUTION ; OOIDS ; MODEL
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
EI主题词2019-10-31
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/310390
作者单位1.King Fahd Univ Petr & Minerals, Coll Petr Engn & Geosci, Geosci Dept, Dhahran 31261, Saudi Arabia;
2.King Fahd Univ Petr & Minerals, Coll Petr Engn & Geosci, Ctr Integrat Petr Res, Dhahran 31261, Saudi Arabia
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Ismanto, Aviandy W.,Chan, Septriandi A.,Babalola, Lamidi O.,et al. Microfacies, biofacies, and depositional environments of the Bajocian-Bathonian Middle Dhruma carbonates, central Saudi Arabia[J],2019,108(8):2577-2601.
APA Ismanto, Aviandy W.,Chan, Septriandi A.,Babalola, Lamidi O.,Kaminski, Michael A.,Al-Ramadan, Khalid A.,&Abdullatif, Osman M..(2019).Microfacies, biofacies, and depositional environments of the Bajocian-Bathonian Middle Dhruma carbonates, central Saudi Arabia.INTERNATIONAL JOURNAL OF EARTH SCIENCES,108(8),2577-2601.
MLA Ismanto, Aviandy W.,et al."Microfacies, biofacies, and depositional environments of the Bajocian-Bathonian Middle Dhruma carbonates, central Saudi Arabia".INTERNATIONAL JOURNAL OF EARTH SCIENCES 108.8(2019):2577-2601.
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