The El Sherana Group is a succession of fluvial and lacustrine sedimentary rocks and bimodal volcanics outcropping in a NW-trending faulted belt in the South Alligator Valley area of the Proterozoic Pine Creek Inlier, Northern Territory, Australia. The El Sherana Group comprises, in ascending stratigraphic order, the Scinto Breccia, Coronation Sandstone, Pu! Pu! Rhyolite and Big Sunday Formation. The Pu! Pu! Rhyolite represents a major period of silicic volcanism during deposition of the El Sherana Group. It contains an association of rhyolitic volcanic, volcaniclastic and intrusive facies, dominated by welded ignimbrites. The volcanic succession is thickest (over I km thick) around the southern margin of the Malone Creek Granite, thinning ...
Contrary to general belief, not all large igneous provinces (LIPs) are characterised by rocks of bas...
The rhyolitic 1071 ± 5 Ma Kathleen Ignimbrite (Formation) forms part of a ~1 km thick, volcanic-sedi...
The Cambra-Ordovician Seventy Mile Range Group occurs as an east-west trending volcano-sedimentary ...
The 1.86 Ga El Sherana/Edith River Basin of Northern Territory, Australia formed during a period of ...
The Ural Volcanics and Mt Hope Volcanics in the Central Lachlan Orogen, New South Wales, overlie non...
The Ural Volcanics and Mt Hope Volcanics in the Central Lachlan Orogen, New South Wales, overlie non...
The Ural Volcanics and Mt Hope Volcanics in the Central Lachlan Orogen, New South Wales, overlie non...
A distinctive Late Ordovician volcano-sedimentary terrane, embracing the Carriers Well Formation and...
The Ural Volcanics are a early Devonian, submarine, felsic lava-sill complex, exposed in the western...
A distinctive Late Ordovician volcano-sedimentary terrane, embracing the Carriers Well Formation and...
A. J. Parker S U M M A RY: Most igneous activity in Australian Proterozoic domains i related to majo...
The Ural Volcanics are a early Devonian, submarine, felsic lava-sill complex, exposed in the western...
Upper Devonian to Lower Carboniferous strata of the Campwyn Volcanics of east central Queensland pre...
Upper Devonian to Lower Carboniferous strata of the Campwyn Volcanics of east central Queensland pre...
The Cambra-Ordovician Seventy Mile Range Group occurs as an east-west trending volcano-sedimentary ...
Contrary to general belief, not all large igneous provinces (LIPs) are characterised by rocks of bas...
The rhyolitic 1071 ± 5 Ma Kathleen Ignimbrite (Formation) forms part of a ~1 km thick, volcanic-sedi...
The Cambra-Ordovician Seventy Mile Range Group occurs as an east-west trending volcano-sedimentary ...
The 1.86 Ga El Sherana/Edith River Basin of Northern Territory, Australia formed during a period of ...
The Ural Volcanics and Mt Hope Volcanics in the Central Lachlan Orogen, New South Wales, overlie non...
The Ural Volcanics and Mt Hope Volcanics in the Central Lachlan Orogen, New South Wales, overlie non...
The Ural Volcanics and Mt Hope Volcanics in the Central Lachlan Orogen, New South Wales, overlie non...
A distinctive Late Ordovician volcano-sedimentary terrane, embracing the Carriers Well Formation and...
The Ural Volcanics are a early Devonian, submarine, felsic lava-sill complex, exposed in the western...
A distinctive Late Ordovician volcano-sedimentary terrane, embracing the Carriers Well Formation and...
A. J. Parker S U M M A RY: Most igneous activity in Australian Proterozoic domains i related to majo...
The Ural Volcanics are a early Devonian, submarine, felsic lava-sill complex, exposed in the western...
Upper Devonian to Lower Carboniferous strata of the Campwyn Volcanics of east central Queensland pre...
Upper Devonian to Lower Carboniferous strata of the Campwyn Volcanics of east central Queensland pre...
The Cambra-Ordovician Seventy Mile Range Group occurs as an east-west trending volcano-sedimentary ...
Contrary to general belief, not all large igneous provinces (LIPs) are characterised by rocks of bas...
The rhyolitic 1071 ± 5 Ma Kathleen Ignimbrite (Formation) forms part of a ~1 km thick, volcanic-sedi...
The Cambra-Ordovician Seventy Mile Range Group occurs as an east-west trending volcano-sedimentary ...