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- | Upper Jurassic ([[Oxfordian]], ~ 152-145 Ma)5 KB (633 words) - 20:02, 18 February 2022
- ...Pentland–Hugin Formation interval is overlain by the thick [[Callovian]]–[[Oxfordian]] age [[Heather Formation]], which is dominated by [[claystone]]s inter-bed16 KB (2,358 words) - 16:28, 11 January 2024
- ...s. Within the trap there are two principal [[reservoir]] units; the late [[Oxfordian]] to early [[Volgian]] Brae member and the “latest” early to middle–l17 KB (2,614 words) - 19:14, 17 January 2022
- ...lovian]]. However, the most active phases of rifting occurred during the [[Oxfordian]] to early [[Volgian]] (early [[Tithonian]]), when very thick [[synrift]] s23 KB (3,562 words) - 19:06, 17 January 2022
- ...to, Sauco, and Isla de la Juventud marbles were deposited over the lower [[Oxfordian]] thin quartzose sandstones of [[La Lamagua Formation|La Llamagua]], [[Loma30 KB (4,263 words) - 22:00, 23 January 2019
- During the Late Callovian, Oxfordian, and Early Kimmeridgian, anoxic conditions prevailed in two intrashelf depr27 KB (3,901 words) - 13:51, 26 January 2017
- Three major Mesozoic source rocks deposited during transgressive events. The Oxfordian Smackover Formation has limestones and marls with an average TOC of 3% and27 KB (3,791 words) - 19:35, 11 October 2022