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Tinga Member

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Journal Article
Journal: GSA Bulletin
Published: 15 March 2018
GSA Bulletin (2018) 130 (9-10): 1474–1492.
..., forming the Tinga Member deposits (phases B-7, C-2, OLT-7). The power and volume of these flood events caused the flow to break out of the Olkesiteti channel, where it reached the Oltepesi Plain, forming a sediment fan with large isolated megaclasts ( Figs. 2 , 5K, and 5L ) and leaving concentrations...
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Image
Overall composite panel diagram for the Oltulelei Formation, looking north,...
Published: 15 March 2018
distances between localities are shown below the panel. Olkesiteti Member is indicated by shades of gray plus the red basal unit in Locality G, Oltepesi Member is indicated by shades of brown, and Tinga Member is indicated by light orange. The Oltulelei Tuffs in the Olkesiteti Member are light gray. Heavy
Image
Summary diagram showing phases of aggradation and erosion in the Olorgesail...
Published: 15 March 2018
lines indicate the time interval between the two formations with no sedimentary record. The Olkesiteti Member filled part of the eroded landscape of the Olorgesailie Formation, the Oltepesi Member filled valleys cut into the previous deposits in the lower parts of this landscape, and the Tinga Member
Image
Perspective view looking north across the Olorgesailie Basin, showing the T...
Published: 15 March 2018
Figure 2. Perspective view looking north across the Olorgesailie Basin, showing the Tinga Member sediment fan and the modern drainage connection into the Naivasha Basin to the north via the Kedong Depression, as well as the Ol Keju Nyiro River, which crosses the basin from east to west before
Image
Representative strata and lithologies of the Oltulelei Formation; see also ...
Published: 15 March 2018
Member 8. (J) Back wall of archaeological excavation BOK-2 showing the disrupted, radiating pattern of a proposed spring vent (within dashed line) in phase B-2, and a clastic dike with pumices, dated at 200 ka ( Table 1 ). (K) Tinga Member boulders of phase B-7 at section B08-04, topping a hill formed
Journal Article
Published: 01 January 2005
Petroleum Geoscience (2005) 11 (1): 79–92.
... compaction relationship b (μs ft −1 ) (m bgl) a Winton Formation Thurakinna-5 142.713 712.759 Δ t =178.493 − 0.0502 dbgl Tinga Tingana-1 153.622 495.629 Mackunda Formation Beanbush-1 106.091 1220.208 Δ t =197.248 − 0.0747 dbgl Fly Lake-1 122.231 1004.255 Allaru...
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Perspective diagrams looking NNE, reconstructing middle to late Pleistocene...
Published: 15 March 2018
) Inferred fault movement on the west side of Locality B, which temporarily blocked east-to-west drainage, filling valleys and depositing distinctive orange-brown sediment over the Oltepesi Plain with distinctive orange-brown sediments (Oltepesi Member). Following this valley filling, a new drainage formed
Journal Article
Published: 01 September 2013
Journal of Paleontology (2013) 87 (5): 842–853.
... are considered in approximate chronologic sequence from oldest to youngest. Anchilestes impolitus Qiu and Li, 1977 , is based on a poorly preserved lower jaw with P 4 -M 3 (IVPP V4315) from the Lower Member of the Wanghudun Formation of Anhui Province, China. The age of these strata was regarded as early...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 28 May 2021
GSA Bulletin (2021)
... margins of Allen and Johnson, 2010; Dooling, 2013; Pet- low Members occurs across the Sevier and Paun- tinga, 2013; Gooley et al., 2016). the Paunsaugunt plateau (Glendale and Tenny saugunt faults (Fig. 7). Within the Paunsaugunt Canyon; Fig. 7), the John Henry Member con- Plateau, the Smoky Hollow Member...
Journal Article
Journal: Economic Geology
Published: 01 January 2017
Economic Geology (2017) 112 (1): 123–143.
... Statistics : Keyworth, Nottingham, UK , British Geological Survey . Brownscombe W. , 2009 , The Tinga anomaly: A new style of gold mineralization in Ghana? : M.Sc. thesis , University of Oxford , 117 p. Caen-Vachette M. , 1988 , Le craton ouest-africain et le bouclier guyanais: un...
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Series: Geological Society, London, Memoirs
Published: 30 October 2020
DOI: 10.1144/M52-018-55
EISBN: 9781786205070