Neoproterozoic–Devonian stratigraphic evolution of the eastern Murzuq Basin, Libya: a tale of tilting in the central Sahara

Abstract

The Murzuq Basin is one of the most petroliferous basins of North Africa. Its remote eastern flank has been largely ignored since early reconnaissance work in the 1950s and 1960s. This article presents new stratigraphic and sedimentological data on the Neoproterozoic through Devonian succession from the Mourizidie and Dor el Gussa regions. The Neoproterozoic to Cambrian Mourizidie and Hasawnah formations in the eastern part of the Mourizidie region dip to the east and north-east, resting directly on late Precambrian metasediments and granitoids. These strata record the initial progradation of sand-dominated braidplain systems upon peneplained Precambrian basement. Rhyolite clasts in the Hasawnah Formation may record tectonically driven uplift and unroofing in the southern Tibesti Massif or tectonomagmatic rejuvenation to the south of this massif. In the western part of the Mourizidie region, Late Ordovician through Silurian strata (Mamuniyat and Tanezzuft-Akakus formations) directly overlie late Precambrian metasediments and granitoids, and dip at a low angle towards the west into the Murzuq Basin. Elsewhere at the eastern Murzuq Basin flank, in Dor el Gussa, Late Ordovician glaciogenic sediments rest with angular unconformity upon shallow marine sandstones of Cambrian-Ordovician age. This angular unconformity may also occur in the Mourizidie region and indicates widespread tectonism, either as a result of a Middle-Late Ordovician orogenic event, far-field tectonism related to the opening of the Rheic Ocean along the northern margin of Gondwana or alternatively crustal depression associated with the growth of Late Ordovician ice sheets. Unconformity development was also probably associated with glacial incision. Following ice sheet retreat, isostatic rebound during deglaciation resulted in uplift of tens to hundreds of metres, locally removing all Cambrian and Ordovician formations. Rising sea levels in the Silurian led to deposition of the Tanezzuft Formation on Precambrian basement in the northwestern Mourizidie region.

Early Palaeozoic evolution of Libya: perspectives from Jabal Eghei with implications for hydrocarbon exploration in Al Kufrah Basin

“…Stratigraphic models for this latter region were recently proposed by Le Heron et al . () and Ghienne et al . ().…”

“…The preponderance of Skolithos in the first lithofacies bears close comparison to the thick intervals of bioturbated sandstone in the Hawaz Formation at Jabal az‐Zalmah (Le Heron & Howard, ) and on the Gargaf Arch (Ramos et al ., ; De Gibert et al ., ). Close similarities are also noted with the Hawaz Formation at the eastern flank of the Murzuq Basin (Ghienne et al ., ; Le Heron et al ., ). We tentatively interpret the large‐scale composite bedforms as tidal bar deposits.…”

“…Clastic‐dominated sedimentation continued during the Devonian and Carboniferous, interrupted by several regional low angle unconformities recording far‐field plate margin events, culminating with the so‐called Hercynian or Mauritanide collision (e.g. Craig et al ., ; Ghienne et al ., ; Le Heron et al ., ).…”

Early Paleozoic tectonic reconstruction of Iran: Tales from detrital zircon geochronology

“…Abbo et al (2015), Dorr et al (2015) and Paquette and Le Pennec (2012) suggested that a high proportion of detrital and xenocrystic zircons with 2.5 to 1.0 Ga ages, both in the Tauride and External Hellenides Neoproterozoic meta-sedimentary successions and in Neogene volcanics from the Eastern Mediterranean, reveal the presence of older "hidden" crustal vestiges along the Cadomian realm. This age peak is common in clastic sediments and so could be recycled from other sedimentary successions (Le Heron et al, 2013, 2015. In fact, the source of these old zircons is an enigma.…”

Insights into crust formation and recycling in North Africa from combined U–Pb, Lu–Hf and O isotope data of detrital zircons from Devonian sandstone of southern Libya

“…A simplified stratigraphic column is shown in Figure 3. Details of the Dor el Gussa stratigraphy are provided in Klitzsch (1964) and Klitzsch & Ziegert (2000), and are summarized in Morton et al (2011) andLe Heron et al (2013).…”