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Tanes Member

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Journal Article
Journal: AAPG Bulletin
Published: 11 October 1997
AAPG Bulletin (1997) 81 (10): 1640-1659.
... by a relatively higher wax content, low sulfur content, a pris- tane/phytane ratio of more than 1.0, a dominance of C 29 steranes, and an abundance of the biomarker gammacerane; the interpretation of these parameters suggests the possibility of two sources for these oils: a siliciclastic marine source...
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Journal Article
Published: 01 October 2009
The Canadian Mineralogist (2009) 47 (5): 1177-1194.
...: (1) early pre-ore tourmaline, and (2) ore-stage tourmaline, which is associated with chamosite. The early-stage tourmaline can be classed as an intermediate member of the schorl–foitite and “oxy-schorl” – “oxy-foitite” series. Its compositions are characterized by their values of X -site vacancy...
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Journal Article
Published: 01 April 2017
Journal of Sedimentary Research (2017) 87 (4): 388-405.
... in the Danian. Sandstones in the Dosados Member (Moreno Fm) are identified as the main parent unit on the basis of total heavy-mineral-assemblage compositions and varietal studies of selected minerals (tourmaline, garnet, titanite, apatite, and zircon). Fluidized sand is emplaced in turbulent flow conditions...
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Journal Article
Published: 01 January 2012
Journal of Paleontology (2012) 86 (1): 25-43.
... the cursorial adaptations seen in later phenacodontids and early perissodactyls. Phylogenetic analysis did not recover monophyletic “Phenacodontidae”; instead, phenacodontids formed a series of sister taxa to the Altungulata clade. Tetraclaenodon is the basal-most member of the “Phenacodontidae” + Altungulata...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1998
AAPG Bulletin (1998) 82 (3): 442-463.
... lean mud shales (TOC <2%). The couplets stack at scales ranging from centimeters to meters. Of particular interest are three black organic-rich mud shales in the middle Velkerri Member, tens of meters thick and correlatable over much of the drilled area of the basin. Their high organic contents...
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Series: GSA Special Papers
Published: 01 January 2007
DOI: 10.1130/2007.2423(13)
...-bentonite layer within an equivalent to the Armorican Quartzite facies in the Cantabrian zone of the Iberian Variscan belt (the Tanes Member of the Barrios Formation), which lies at the Tremadocian-Floian boundary (global Ordovician chronostratigraphy updated by the International Commission of Stratigraphy...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 2011
AAPG Bulletin (2011) 95 (3): 339-370.
... for a variety of companies in exploration programs in New Zealand, Australia, Thailand, Philippines, Malaysia, and Canada, including roles as chief geologist at Petrocorp Exploration and exploration manager at Santos and TAG Oil. He is a member of the Petroleum Exploration Society of Australia and has been...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1996
AAPG Bulletin (1996) 80 (8): 1216-1241.
... = mudstone, thick dashes = coal, dots = sandstone, wiggles = marl, brick patterns = limestone, v = volcaniclastics. Bold numbers represent matrix thermal conductivities (in W/m/K) determined from the lithologic end members for the representative units in the wells listed above the column. Matrix thermal...
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Journal Article
Journal: AAPG Bulletin
Published: 11 October 1994
AAPG Bulletin (1994) 78 (10): 1560-1585.
... in Figures 10 and 11 also shown. Ari = Ariki-1, Awk = Awakino-1, Fre = Fresne-1, Kai = Kaimiro-1 and 2, KDp = Kapuni Deep-1, Kpe = Kupe-1, KS4 = Kupe South-4, McK = McKee-1 and 3A, NP2 = New Plymouth-2, Tne = Tane-1, Tng = Tangaroa-1, Wai = Waihapa-1 and 2, Wit = Witiora-1; see Table 2 for other well...
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Series: GSA Field Guide
Published: 01 January 2005
DOI: 10.1130/2005.fld006(08)
EISBN: 9780813756066
... of Tertiary rocks in the Third Creek Member. The Paleocene to Eocene Wasatch Formation, late Miocene to Pliocene Salt Lake Formation, and Pliocene-Pleistocene(?) piedmont gravel deposits overlie the Paleozoic and older rocks along an angular unconformity (Fig. 6 ). The distinctive lithologies...
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Journal Article
Published: 11 March 2019
Geological Magazine (2019) 156 (10): 1751-1770.
... and the weathered glauconitic Oligocene Matapo Sandstone Member, Pillar Point, NW Nelson. Hammer for scale is 40 cm long. (c) Toru-1, 3765.4 m, Matapo Sandstone Member: thin-section view of a highly glauconitic sandstone with subordinate quartz, feldspar and lithic fragments. (d) Onaero-1, 3478 m, Matapo Sandstone...
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Series: Geological Society, London, Geology of Series
Published: 01 January 2002
DOI: 10.1144/GOSPP.4
EISBN: 9781862393912
... ; Robardet 1981 ; Rodríguez Núñez et al. 1989 ; García Palacios et al. 1996 ) that are also known in most areas of the Iberian Peninsula as well as in the other regions of the North Gondwanan shelf. In the Guadarranque syncline, a black shale intercalation in the middle quartzitic member of the Gualija...
Journal Article
Journal: GSA Bulletin
Published: 01 May 2007
GSA Bulletin (2007) 119 (5-6): 725-742.
...-grained sandstone (Wairere Member) and mudstone (Maori Bay Member) with interbedded tuffs. Distal apron deposits occur between the northernmost part of the apron along the coast between S2 and S7. The medial apron consists of thicker, pumiceous or pebbly sandstone interbedded with intervals of fine...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 2001
AAPG Bulletin (2001) 85 (8): 1469-1498.
... of Wellington, New Zealand, in 1983. Since then he has worked as an exploration and development geologist in Australia, New Zealand, southeast Asia, and Pakistan. He is a member of AAPG, the Society of Petroleum Engineers, and the Society of Professional Well Log Analysts. He maintains an interest in calcareous...
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Journal Article
Published: 13 May 2016
Geological Magazine (2017) 154 (4): 661-682.
... Campanian–Maastrichtian Cape Farewell-1 drillhole, offshore NW Nelson at 2430' 40°29', 172°40' 7a TANE-1-Mh 24724a Pakawau Group sm Campanian Tane-1 drillhole, offshore Taranaki at 3928m 38°56', 172°38' 7b TANE-1-Rt 24724b Pakawau Group sm Campanian Tane-1 drillhole, offshore Taranaki...
Journal Article
Published: 01 July 2000
Journal of Foraminiferal Research (2000) 30 (3): 246-249.
... to Beggiatoa, existed during that time. Here we report on the eukaryotic community of a modern analogue, the Santa Barbara Basin (California, USA). The Beggiatoa mats of these severely dysoxic and sulphidic: sediments support a surprisingly abundant protistan and metazoan meiofaunal community, most members...
Journal Article
Published: 14 February 2006
Canadian Journal of Earth Sciences (2005) 42 (12): 2195-2216.
... units to member status. We define the Tabia Member (a town in the Oulili river where the Tabia Member is developed best, MS-8, Fig.  2 ) as the 0–250 m of peritidal carbonates, evaporites, mudcracked siltstones, fluvial sandstones, and coarse siliciclastic debris that was deposited in a series of linked...
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Journal Article
Published: 01 May 2012
Bulletin de la Société Géologique de France (2012) 183 (3): 233-249.
... (megasequence I) of Kerrouchen basin (G1). mi: lower member with coarse sandy-conglomerate; mm: middle member with sandstones and siltstones; ms: Upper member with red evaporitic clays (central part of the basin); 2: “Muds cracks” superimposed to the asymetric ripple marks at top of the sandstone level (mi...
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Journal Article
Published: 01 December 2002
Journal of Micropalaeontology (2002) 21 (2): 115-130.
...) reflects the gonyaulacoid dinocyst dominance. Abundance of proximate dinocysts is highest in shallow-water intervals, e.g. c. 2950–2500 m. No foraminifera were recovered from the Bara Member, Ranikot Formation. Therefore palaeobathymetry/distance from shore determinations are palynologically based...
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Journal Article
Published: 01 October 2007
Journal of Micropalaeontology (2007) 26 (2): 127-143.
... genera and families of shallowwater (<100 m) benthic foraminifera from around northeast North, South, Stewart, Chatham, Snares, Auckland and Campbell Islands. A different pattern emerges in the shallow-water members of the Rosalinidae, with similar levels of species richness (13–14 spp.) off...
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