... psammitic enclaves of the Woodburn Lake group within 1.83 Ga Hudson granite and Martell syenite that together comprise the Shultz Lake intrusive complex (SLIC). The depth and geometry of the intrusive complex are relatively unknown as the geological constraints are poor; the drilling is sparse...

... the diverse nature of the depositional products of the Jackfork Group, especially at DeGray Lake Dam and Spillway and Kiamichi Mountain. They pointed out sandy and muddy debrites and thin- to medium-bedded turbidites (or turbidite-like) beds with and without current-reworked tops, in addition to slumps...

... Tres Pasos Formation (deep-water upper-slope turbidites and mass-transport deposits; Katz 1963 ; Shultz et al. 2005 ; Romans et al. 2008b ; Armitage et al. 2009 ) to the Dorotea Formation (shallow-water shelfal and deltaic deposits; Katz 1963 ) in the Magallanes foreland basin ( Figs. 1 , 2...

... outer 24 complex 455 190 — 4 outer − >> 200 inner 7.5 inner 7.5 concentric inner − Tvären 2 inner 2 outer? eroded simple concentric? 457 65 — ? ? eroded 100–150 Kamensk 20 outer 38 complex 65 700 — 12 — 100–200 inner 20 concentric...

... on or above the sub-Cretaceous unconformity surface occurred throughout Mannville Group deposition. These paleovalleys range in scale from major conduits (10’s of km wide and >40 m deep), to smaller features (5 km wide and 25 m deep; e.g. Zaitlin and Shultz, 1984 ) associated with local topographic relief...

... , Facies architecture of a submarine fan channel–levee complex: the Juniper Ridge Conglomerate, Coalinga, California : Sedimentology , v. 49 , p. 335 – 362 . Hubbard , S.M. , and Shultz , M.R. , 2008 , Deep burrows in submarine fan-channel deposits of the Cerro Toro Formation (Cretaceous...

... succession by Hilbert-Wolf et al. (2015, 2017) and Mtelela et al. (2016 , 2017 ) established age constraints and preliminary stratigraphic and sedimentological context for the overlying Lake Beds succession, a complex alluvial–lacustrine succession deposited intermittently between 8.7 Ma to 5 ka...

... deposition of Associations 2 and 3, recording proglacial lacustrine deposition in the Gateway area. B) Depicts filling of the lake and either fluvial bypass or nominal fluvial aggradation. C) Depicts aggradation of the fluvial system, and backfilling toward ancestral Unaweep Canyon. The fluvial system...