1-20 OF 72 RESULTS FOR

Hibernia Sandstone Member

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1989
AAPG Bulletin (1989) 73 (5): 557–575.
.... , and R. W. Yole , 1985 , Sedimentology of the Hibernia member, Missisauga formation, within the Hibernia oil field (abs.) : Geological Association of Canada Program with Abstracts , v. 10 , p. A7 . Brown , D. M. , and R. W. Yole , 1988 , Cathodoluminescence and sandstone...
FIGURES | View All (17)
Journal Article
Published: 01 December 1993
Bulletin of Canadian Petroleum Geology (1993) 41 (4): 389–406.
... lithostratigra- phy; note basinal seals (e.g., Nautilus Shale, Whiterose Shale, Fortune Bay Shale), reservoirs (Catalina, Ben Nevis, Avalon, Hibernia, Jeanne d'Arc formations) and source rock intervals (Egret Member, Voyager and Jeanne d'Arc formations), together with an indication of hydrocarbon occurrences...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 2005
AAPG Bulletin (2005) 89 (9): 1203–1237.
...; Figures 2– 4 ). From the Early to Late Jurassic (Kimmeridgian), sedimentation was dominated by shallow-marine sandstone, shale, and limestone in an epeiric sea ( Grant and McAlpine, 1990 ). The upper part of this shallow-marine section includes the Egret Member of the Rankin Formation, the richest...
FIGURES | View All (21)
Journal Article
Published: 01 June 1994
Bulletin of Canadian Petroleum Geology (1994) 42 (2): 268–271.
... that they make no contribu- tion to overpressures (figure 14). 4.4 On page 404 the authors tate: "In the Hibernia Fault block, the Egret source became overpressured at 130 Ma .. . . " However, according to figure 14, the Egret Member became overpressured at 140 Ma. Two sentences below they state: "A rapid...
Journal Article
Journal: GSA Bulletin
Published: 01 March 2014
GSA Bulletin (2014) 126 (3-4): 600–614.
...David P. West, Jr.; Richard N. Abbott, Jr.; Betsy R. Bandy; Michael J. Kunk Abstract Two fault-bounded sequences of metamorphic rocks are exposed in the Blue Mountains of eastern Jamaica. Westphalia Schist is dominated by amphibolite facies hornblende schist and mica schist. Mt. Hibernia Schist...
FIGURES | View All (9)
Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2006
DOI: 10.1306/1215878M883271
EISBN: 9780891813699
... sandstones of the Burgan Formation below to low net/gross marine mud-stones, sandstones, and limestones of the Mauddud Formation above. Within this context, fine-grained siliciclastics, traditionally included at the top of the Burgan Formation to the south, are assigned to the clastic member of the Mauddud...
FIGURES | View All (23)
Journal Article
Published: 01 July 1981
Journal of the Geological Society (1981) 138 (4): 375–405.
.... ‘Londinia’ exposes mostly Old Red Sandstone, Lower Carboniferous and Upper Jurassic; Cornubia-New Red Sandstone and Upper Jurassic; Armorica-Precambrian, New Red Sandstone and Jurassic (with Middle Jurassic igneous rocks or pyroclastics); Hibernia-Lower and Upper Palaeozoic. Contemporary volcanicity...
Series: GCSSEPM, GCSSEPM
Published: 01 December 2012
DOI: 10.5724/gcs.12.32.0598
EISBN: 978-0-9836097-8-0
... of exploration in the 1960’s, regional exploration on the Grand Banks has been primarily focused on the Early Cretaceous Ben Nevis and Hibernia formations shallow marine sandstone reservoirs. This early phase of exploration resulted in the discovery of the Hibernia, White Rose, and Hebron fields in the southern...
FIGURES | View All (7)
Journal Article
Journal: AAPG Bulletin
Published: 01 July 2000
AAPG Bulletin (2000) 84 (7): 1015–1040.
...Alaa M. Salem; S. Morad; Luiz F. Mato; I. S. Al-Aasm Abstract The reservoir quality of fluvial sandstones of the Upper Jurassic Boipeba Member, Recôncavo basin, northeastern Brazil, is highly heterogeneous and controlled by eodiagenesis under semiarid climate, mesodiagenesis during burial...
FIGURES | View All (21)
Series: GCSSEPM, GCSSEPM
Published: 01 December 1994
DOI: 10.5724/gcs.94.15.0115
EISBN: 978-0-9836097-5-9
... flowing turbidity currents that deposited sandstones encountered in wells on the northern part of the Outer Ridge ( DeSilva 1993a ). Rich Kimmeridgian source rocks, the Egret Member of the Rankin Formation, were deposited during this time. A regional erosional unconformity, the Tithonian Unconformity...
Journal Article
Journal: AAPG Bulletin
Published: 11 December 1999
AAPG Bulletin (1999) 83 (12)
... and 170 x 10 9 m 3 (6 Tcf) of natural gas, mainly from the mature Western Canada Sedimentary Basin. In the next millennium, expanded contributions to production capacity will come initially from the Mesozoic Jeanne d’Arc Basin (e.g. Hibernia & Terra Nova oil) offshore Newfoundland and basins off Nova...
FIGURES | View All (12)
Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2001
DOI: 10.1306/M74775C8
EISBN: 9781629810621
... 3 (300 million bbl), insufficient for an initial development. Grand Banks (Jeanne d’Arc Basin) assessments are supported by rich Jurassic source rock (Egret) and the discoveries to date (Hibernia, etc.). Vast resources await investment and extraction in the Alberta oil sands. Only 447 million m 3...
FIGURES | View All (12)
Series: AAPG Hedberg Series, AAPG Hedberg Series
Published: 01 January 2012
DOI: 10.1306/13311442H43475
EISBN: 9781629810003
.... (1989) . In the eastern part of the study area, the Egret Member splits into a Lower and Upper Kimmeridgian source rock separated by a sandstone interval ( Magoon et al., 2005 ). The source rock consists of laminated brown marl and calcareous shale as well as lime and mudstone with a high organic...
FIGURES | View All (22)
Journal Article
Journal: AAPG Bulletin
Published: 01 September 2003
AAPG Bulletin (2003) 87 (9): 1459–1483.
... ). The easternmost limit of the Otter Bay Member, as used here, defines an arbitrary eastern limit for both the Red Island and Bay Bulls members ( Figure 5 ). The Otter Bay Member (type section: Hibernia J-34, 1482–1591 m; Sinclair, 1988 ) ( Table 1 ) is a sandstone unit located along the western margin...
FIGURES | View All (11)
Journal Article
Published: 01 June 1992
Bulletin of Canadian Petroleum Geology (1992) 40 (2): 136–150.
... drilled to date are shown. EGRET MEMBER SOURCE ROCK, JEANNE d'ARC BASIN 139 m o. 10- o 2o- ~o-p_+ } . 70- I tO - 11o- . 170- ~00- 210- 24O- CORMORANT N-83 RANKIN M-36 l EGRET BEN NEVIS 1-45 HIBERNIA POSITIONAL AGE SPOONBILLC-30 MURRE G-67 N-46 K-36 I CE HEBRON 1-13 0-35 K-181 ;EQUENCE TO 2T57m ~ O...
Journal Article
Journal: AAPG Bulletin
Published: 01 October 2000
AAPG Bulletin (2000) 84 (10): 1617–1632.
... Member of the Hibernia K-18 section has the highest frequency of persistent major cycles (~4.5 m) and, consequently, gives n max = 19.5 and, according to equation 7 , the longest accumulation time of all sections investigated ( t a = 1.95 m.y.). According to equation 4 , the stratigraphic...
FIGURES | View All (10)
Series: GCSSEPM, GCSSEPM
Published: 01 December 1996
DOI: 10.5724/gcs.96.17.0341
EISBN: 978-0-9836097-6-6
... of the HST (Otter Bay and Fox Harbour Members of Fig. 2 ) and the LST (Mara sandstone, Fig. 2 ) are shown in the isochron maps ( Fig. 5 ). Figure 2. Lithostratigraphy of post-Late Cretaceous sequences in the Jeanne d’Arc Basin (adapted from de Silva 1993 ). The eu static sea-level curve is from...
Journal Article
Journal: AAPG Bulletin
Published: 01 December 2005
AAPG Bulletin (2005) 89 (12): 1593–1606.
... layers intercalated with silty and clay-rich beds. We will focus on the porous sandstones in the footwall of the fault because they are most relevant to the petroleum industry and can more easily be compared to other examples in the same area. Two stratigraphic units, the Slick Rock Member...
FIGURES | View All (16)
Journal Article
Published: 01 January 2015
Journal of Sedimentary Research (2015) 85 (1): 62–81.
...Greg M. Baniak; Murray K. Gingras; Beverly A. Burns; S. George Pemberton A bstract : A petrophysical study of bioturbated shoreface sandstone rocks was completed by mapping local variations in air permeability measured in core samples acquired from the Upper Jurassic Ula Formation of the Norwegian...
FIGURES | View All (14)
Journal Article
Journal: AAPG Bulletin
Published: 01 August 2010
AAPG Bulletin (2010) 94 (8): 1093–1132.
...Thomas R. Taylor; Melvyn R. Giles; Lori A. Hathon; Timothy N. Diggs; Neil R. Braunsdorf; Gino V. Birbiglia; Mark G. Kittridge; Calum I. Macaulay; Irene S. Espejo Abstract Models and concepts of sandstone diagenesis developed over the past two decades are currently employed with variable success...
FIGURES | View All (28)