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Naskapi Formation

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Journal Article

Correlation of the Aptian Naskapi Member of the Scotian Basin and its regional implications

Isabel Chavez, David J.W. Piper, Georgia Pe-Piper
Published: 26 February 2018
Canadian Journal of Earth Sciences (2018) 55 (5): 514–535.
DOI: https://doi.org/10.1139/cjes-2017-0205
...Isabel Chavez; David J.W. Piper; Georgia Pe-Piper The Naskapi Member of the Logan Canyon Formation, a 150 m thick shale-dominated unit, lies in between sand-dominated units of Upper Missisauga Formation below and the Cree Member above. The great decrease in sediment supply has been suggested as due...
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Correlation of COST G-2, <span class="search-highlight">Naskapi</span> N-30, and Cree E-35 wells. Allostratigraph...

Correlation of COST G-2, Naskapi N-30, and Cree E-35 wells. Allostratigraph...

Published: 26 February 2018
Fig. 7. Correlation of COST G-2, Naskapi N-30, and Cree E-35 wells. Allostratigraphic surfaces: marker A, top of the Upper Missisauga Formation; marker B, base of the shales of the Naskapi Member; marker C, Intra-Aptian maximum flooding surface; and marker D, top of the Naskapi Member. [Colour
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Correlation of Glenelg J-48, Eagle D-21, and South Griffin J-13 wells. Allo...

Correlation of Glenelg J-48, Eagle D-21, and South Griffin J-13 wells. Allo...

Published: 26 February 2018
Fig. 4. Correlation of Glenelg J-48, Eagle D-21, and South Griffin J-13 wells. Allostratigraphic surfaces: marker A, top of the Upper Missisauga Formation; marker B, base of the shales of the Naskapi Member; marker C, Intra-Aptian maximum flooding surface; and marker D, top of the Naskapi Member
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Correlation of the Sable Island C-67, Penobscot L-30, and Dover A-43 wells....

Correlation of the Sable Island C-67, Penobscot L-30, and Dover A-43 wells....

Published: 26 February 2018
Fig. 5. Correlation of the Sable Island C-67, Penobscot L-30, and Dover A-43 wells. Allostratigraphic surfaces: marker A, top of the Upper Missisauga Formation; marker B, base of the shales of the Naskapi Member; marker C, Intra-Aptian maximum flooding surface; and marker D, top of the Naskapi
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Correlation of the Penobscot L-30, West Esperanto B-78, and Hesper I-52 wel...

Correlation of the Penobscot L-30, West Esperanto B-78, and Hesper I-52 wel...

Published: 26 February 2018
Fig. 6. Correlation of the Penobscot L-30, West Esperanto B-78, and Hesper I-52 wells. Allostratigraphic surfaces: marker A, top of the Upper Missisauga Formation; marker B, base of the shales of the Naskapi Member; marker C, Intra-Aptian maximum flooding surface; and marker D, top
Journal Article

Sedimentology and stratigraphy of a thick, areally extensive fluvial–marine transition, Missisauga Formation, offshore Nova Scotia, and its correlation with shelf margin and slope strata

Don I. Cummings, Bruce S. Hart, R. William C. Arnott
Published: 01 June 2006
Bulletin of Canadian Petroleum Geology (2006) 54 (2): 152–174.
DOI: https://doi.org/10.2113/gscpgbull.54.2.152
... data. The succession consists of 50 m of dune cross-stratified sandstone overlain by 50 m of tide-influenced heterolithic strata, which in turn is overlain by 150 m of mudstone of the Naskapi Member of the Logan Canyon Formation. The succession is interpreted to be a fluvial–marine transition formed...
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Journal Article

SALT DIAPIRS AND THERMAL MATURITY: SCOTIAN BASIN

C. E. Keen
Published: 01 June 1983
Bulletin of Canadian Petroleum Geology (1983) 31 (2): 101–108.
DOI: https://doi.org/10.35767/gscpgbull.31.2.101
... Z: 1 = I.~ t T t* t'~ t - - " -h .~ ~ . . . . . . . . . . . . . . . . I e i . TOP VERRiLL 25 CANYON . . . . ++ 1 7 5 ° ~ a" 6 ; ; ;~ ; ;L~; i i i~2* Fig. 4. Results of calculations for the West Sable structure. The positions of the top of the Verrill Canyon and Naskapi Formations are shown, as well...
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Correlation of the Cree E-35, Glenelg J-48, and Whycocomagh N-90 wells. Int...

Correlation of the Cree E-35, Glenelg J-48, and Whycocomagh N-90 wells. Int...

Published: 26 February 2018
Fig. 3. Correlation of the Cree E-35, Glenelg J-48, and Whycocomagh N-90 wells. Interpretation of depositional environment based on wireling log response, lithostratigraphy, biostratigraphy, and key sequence surfaces. Allostratigraphic surfaces: marker A, top of the Upper Missisauga Formation
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Correlation of the Panuke B-90, Cree E-35, and Cohasset L-97 wells. The cor...

Correlation of the Panuke B-90, Cree E-35, and Cohasset L-97 wells. The cor...

Published: 26 February 2018
Scotia Offshore Petroleum Board. Allostratigraphic surfaces: marker A, top of the Upper Missisauga Formation; marker B, base of the shales of the Naskapi Member; marker C, Intra-Aptian maximum flooding surface; and marker D, top of the Naskapi Member. [Colour online.]
Journal Article

Stratigraphic Framework and Petroleum Potential of Northeastern Baltimore Canyon Trough, Mid-Atlantic Outer Continental Shelf

Jan Libby-French
Journal: AAPG Bulletin
Published: 01 January 1984
AAPG Bulletin (1984) 68 (1): 50–73.
DOI: https://doi.org/10.1306/AD460968-16F7-11D7-8645000102C1865D
... and delta-front sand and shale, equivalent to the Scotian Shelf Missisauga Formation, were deposited. A destructional phase of the delta is represented by the Naskapi equivalent, a calcareous shale. Inundation by the sea was incomplete, however, and channel and distributary-mouth-bar sands (Logan Canyon...
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Variation in V, Nb, and Zr in detrital rutile and anatase (type A) plotted ...

Variation in V, Nb, and Zr in detrital rutile and anatase (type A) plotted ...

Published: 15 June 2019
Figure 11. Variation in V, Nb, and Zr in detrital rutile and anatase (type A) plotted against stratigraphic column for the Continental Offshore Stratigraphic Test G-2 well. Lithology legend is in Figure 2 . CENO. = Cenomanian; E = Early; Fm = Formation; KB = Kelly Bush; Mb = Member; Nask
Journal Article

Single-grain detrital-muscovite ages from Lower Cretaceous sandstones, Scotian basin, and their implications for provenance

Peter H. Reynolds, Georgia Pe-Piper, David J.W. Piper, A.M. Grist
Published: 01 March 2009
Bulletin of Canadian Petroleum Geology (2009) 57 (1): 63–80.
DOI: https://doi.org/10.2113/gscpgbull.57.1.63
... the Sable Island transect (ca. 240 Ma) is much lower than that from the Chaswood Formation (ca. 365 Ma, adjusted to conform to revised ages of standards). The relatively narrow distribution of ages from the Naskapi N-30 well (Fig. 4B ) falls within the Chaswood Formation distribution at the high end...
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Stratigraphic columns from the studied wells showing stratigraphic location...

Stratigraphic columns from the studied wells showing stratigraphic location...

Published: 01 March 2009
Fig. 2. Stratigraphic columns from the studied wells showing stratigraphic location of samples. Stratigraphic detail shown only for the Lower Cretaceous. Stratigraphic picks from MacLean and Wade (1993) ; note that they did not further subdivide the Logan Canyon Formation in the MicMac J-77
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Modal abundance of detrital heavy minerals against the stratigraphic column...

Modal abundance of detrital heavy minerals against the stratigraphic column...

Published: 15 June 2019
are based on the International Biostratigraphers Inc. (unpublished results) and Nova Scotia Department of Energy (2015) (NSDoE). Porosity and permeability of sands are based on sidewall cores from Amato and Simonis (1980) . ρb = formation bulk density (log reading); FM = Formation; HM = heavy minerals
Journal Article

Detrital zircon geochronology and polycyclic sediment sources, Upper Jurassic – Lower Cretaceous of the Scotian Basin, southeastern Canada 1 This article is one of a series of papers published in this CJES Special Issue on the theme of Mesozoic–Cenozoic geology of the Scotian Basin .

David J.W. Piper, Georgia Pe-Piper, Mike Tubrett, Stavros Triantafyllidis, Greg Strathdee
Published: 19 November 2012
Canadian Journal of Earth Sciences (2012) 49 (12): 1540–1557.
DOI: https://doi.org/10.1139/e2012-072
...., Cretaceous; Jur., Jurassic. In the Cree Member of the Logan Canyon Formation (Albian) at the Alma K-85 well, in the western part of the Sable Subbasin, the principal probability peaks are at 350–400 Ma, 550–650 Ma, ∼1.0 Ga, ∼1.2 Ga, and ∼1.65 Ga. It differs from the sample from the Naskapi N-30 well...
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Journal Article

GEOLOGY OF THE WEST SABLE STRUCTURE

H. A. Smith
Published: 01 March 1975
Bulletin of Canadian Petroleum Geology (1975) 23 (1): 109–130.
DOI: https://doi.org/10.35767/gscpgbull.23.1.109
... shale units, the Naskapi and Sabl e shales, thin to the north. An eroded, faulted or nondeposited Wyandot Chalk is suggested in the vicinity of some diapiric features . Major lithologies of the formations are shown as well as significant shows an d gross pay sections. Two types of diapiric structures...
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A revised biostratigraphic and well-log sequence-stratigraphic framework for the Scotian Margin, offshore eastern Canada 1 This article is one of a series of papers published in this CJES Special Issue on the theme of Mesozoic–Cenozoic geology of the Scotian Basin . 2 Earth Sciences Sector Contribution 20120137.

Janice F. Weston, R. Andrew MacRae, Piero Ascoli, M. Kevin E. Cooper, Robert A. Fensome, David Shaw, Graham L. Williams
Published: 25 November 2012
Canadian Journal of Earth Sciences (2012) 49 (12): 1417–1462.
DOI: https://doi.org/10.1139/e2012-070
... and Wade 1975 ). The Logan Canyon Formation is composed of sandstones and shales, with some parts predominantly sandstone (the younger Marmora Member and the older Cree member), and some parts predominantly shale (the younger Sable Member and the older Naskapi Member). In the Barremian to Valanginian...
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Early Cretaceous volcanism in the Scotian Basin 1 This article is one of a series of papers published in this CJES Special Issue on the theme of Mesozoic–Cenozoic geology of the Scotian Basin .

Sarah J. Bowman, Georgia Pe-Piper, David J.W. Piper, Robert A. Fensome, Edward L. King
Published: 20 November 2012
Canadian Journal of Earth Sciences (2012) 49 (12): 1523–1539.
DOI: https://doi.org/10.1139/e2012-063
... the Naskapi Member of the Logan Canyon Formation ( MacLean and Wade 1993 ). Fig. 7. Stratigraphic columns and correlation of the Orpheus Graben wells and Hesper I-52. Also shows summary of new palynological biostratigraphy. In the Jason C-20 well, the lower volcanic unit directly overlies...
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The provenance of Middle Jurassic sandstones in the Scotian Basin: petrographic evidence of passive margin tectonics 1 This article is one of a series of papers published in this CJES Special Issue on the theme of Mesozoic–Cenozoic geology of the Scotian Basin . 2 Geological Survey of Canada Contribution 20110319.

Gang Li, Georgia Pe-Piper, David J.W. Piper
Published: 29 October 2012
Canadian Journal of Earth Sciences (2012) 49 (12): 1463–1477.
DOI: https://doi.org/10.1139/e2012-061
... of tourmaline is similar in the four Jurassic Mohican Formation samples. Type 4 is predominant, followed by type 1, with types 2 and 3 rare or absent. This assemblage is similar to that in Cretaceous sandstones from the wells Naskapi N-30, Musquodoboit E-23, and Alma K-85 ( Fig. 6 ). It is different from...
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The provenance of Jurassic and Lower Cretaceous clastic sediments offshore southwestern Nova Scotia

Dan-Cezar Dutuc, Georgia Pe-Piper, David J.W. Piper
Published: 01 September 2016
Canadian Journal of Earth Sciences (2017) 54 (1): 33–51.
DOI: https://doi.org/10.1139/cjes-2016-0109
... concentrations in trace elements (Zr, Nb, Cr, Ce, and Ta) ( Figs. 10B–10E ) and REE patterns ( Fig. 12 ) as one shale sample from the Lower Cretaceous Missisauga Formation at Naskapi N-30. As noted earlier in the text for tourmaline, this interval in Naskapi N-30 shows exclusive derivation from the Meguma...
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