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BIOSTRAT

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Series: GCSSEPM
Published: 01 December 2000
DOI: 10.5724/gcs.00.15.0116
EISBN: 978-0-9836097-0-4
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Stratigraphy of the Saint-Pons stromatactis carbonate mounds.  A)  <b>Biostrat</b>...
Published: 01 July 2012
F ig 2— Stratigraphy of the Saint-Pons stromatactis carbonate mounds. A) Biostratigraphic, lithostratigraphic, and sequence stratigraphic framework of the Upper Calcareous Member that contains the Saint-Pons stromatactis carbonate mounds. Stratigraphy, ages, depositional sequences, and interpre
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Chronostratigraphic correlation of the Lower Greensand Group using <b>biostrat</b>...
Published: 01 May 2010
Figure 3 Chronostratigraphic correlation of the Lower Greensand Group using biostratigraphic information compiled from a variety of sources, including: Casey (1961) , Owen ( 1972 , 1992 ), Rawson et al. (1978) , Gallois ( 1988 , 1994 ), Hesselbo et al. (1990a) , Hesselbo et al. (1990b) , Ru
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Chronostratigraphic correlation of the Lower Greensand Group using <b>biostrat</b>...
Published: 01 May 2010
Figure 3 Chronostratigraphic correlation of the Lower Greensand Group using biostratigraphic information compiled from a variety of sources, including: Casey (1961) , Owen ( 1972 , 1992 ), Rawson et al. (1978) , Gallois ( 1988 , 1994 ), Hesselbo et al. (1990a) , Hesselbo et al. (1990b) , Ru
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APPENDIX 3  <b>Biostrat</b> modeling parameters
in > PALAIOS
Published: 01 April 2002
APPENDIX 3  Biostrat modeling parameters
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F ig . 3. Map of the Deborah anticline, showing more detail of the <b>biostrat</b>...
Published: 01 March 2002
F ig . 3. Map of the Deborah anticline, showing more detail of the biostratigraphic units and anticlines. Map modified from a portion of the Golden Square 1:10000 map accompanying the Bendigo gold field, Geological Survey of Victoria Report 93 ( Willman and Wilkinson, 1992 ).
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Figure 2. Position of U-Pb dated tuff layer (heavy black line) and <b>biostrat</b>...
in > Geology
Published: 01 January 2000
Figure 2. Position of U-Pb dated tuff layer (heavy black line) and biostratigraphy of Triassic-Jurassic boundary section on Kunga Island. Occurrences of key radiolarian (R), conodont (C), and ammonite (A) taxa and section measurements are compiled from published data ( Tipper et al., 1994 ; Carter,
Series: GCSSEPM
Published: 01 December 2012
DOI: 10.5724/gcs.12.32.0133
EISBN: 978-0-9836097-8-0
Journal Article
Published: 01 July 2012
Journal of Micropalaeontology (2012) 31 (2): 189-192.
Journal Article
Journal: Palynology
Published: 01 January 2000
Palynology (2000) 24 (1): 21-35.
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Journal Article
Journal: Palynology
Published: 01 January 2000
Palynology (2000) 24 (1): 79-93.
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Journal Article
Journal: Palynology
Published: 01 October 1990
Palynology (1990) 14 (1): 135-144.
Journal Article
Published: 30 March 1988
Micropaleontology (1988) 34 (1): 63-66.
... addresses recent and pending refinements in the genus and species taxonomy of biostrat-igraphically significant fossil groups, the potential they hold for greatly improved correlation, and the obstacles to be overcome for that potential to be realized. A solid foundation for biostratigraphic...
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Journal Article
Published: 01 January 2005
Rocky Mountain Geology (2005) 40 (1): 1-24.
... estuarine environments. Biostratal alternations between fresh- and brackish-water assemblages indicate that the Tongue River Member was deposited along a low-gradient coastal plain that was repeatedly inundated from the east by the Cannonball Sea. The existence of marine-influenced beds in the Tongue River...
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Journal Article
Journal: Geology
Published: 01 May 1994
Geology (1994) 22 (5): 431-434.
... by which this curve was constructed. Strictly standardized 87 Sr/ 86 Sr ratios and biostrat igraphic data for ∼1300 87 Sr/ 86 Sr analyses of marine minerals were input into a data base. Objective criteria were used to assign each data point a reliability score. These scores were used as initial weights...
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Log of drill core HS showing facies of Virgin Hills Formation overlying Gog...
in > Geology
Published: 01 April 2014
). Depositional ages are constrained by conodont biostratigraphy (Biostrat.; arrows show samples) using Frasnian MN (Montagne Noire) zonal scheme. Two main extinction levels are shown in blue. Intervals with elevated TOC are shown in yellow (TOC1–TOC3). EX1, EX2, and EX3 are positive δ 13 C excursions. TOC1
Journal Article
Journal: The Leading Edge
Published: 01 January 2012
The Leading Edge (2012) 31 (1): 84-88.
... and gravimetric surveys; outcrop samples; palynology and biostrat; plus much more. These studies were completed primarily for siting new high-hazard nuclear and research facilities and to support long-term environmental stewardship. After looking across all data, particularly in the deep geophysical borings...
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Journal Article
Journal: PALAIOS
Published: 01 April 2002
PALAIOS (2002) 17 (2): 134-146.
...APPENDIX 3  Biostrat modeling parameters ...
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Journal Article
Journal: Geology
Published: 01 April 2014
Geology (2014) 42 (4): 327-330.
... ). Depositional ages are constrained by conodont biostratigraphy (Biostrat.; arrows show samples) using Frasnian MN (Montagne Noire) zonal scheme. Two main extinction levels are shown in blue. Intervals with elevated TOC are shown in yellow (TOC1–TOC3). EX1, EX2, and EX3 are positive δ 13 C excursions. TOC1...
FIGURES