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Hornerstown Formation
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1-20 OF 67 RESULTS FOR
Hornerstown Formation
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Journal Article
Maastrichtian ammonites from the Hornerstown Formation in New Jersey
Journal: Journal of Paleontology
Publisher: Paleontological Society
Published: 01 September 1996
Journal of Paleontology (1996) 70 (5): 798–804.
Journal Article
Paleoecology and morphologic variation of a Paleocene terebratulid brachiopod (Oleneothyris harlani) from the Hornerstown Formation of New Jersey
Journal: Journal of Paleontology
Publisher: Paleontological Society
Published: 01 January 1977
Journal of Paleontology (1977) 51 (1): 86–107.
Journal Article
REE Signatures in Vertebrate Fossils from Sewell, NJ: Implications for Location of the K-T Boundary
Journal: PALAIOS
Publisher: SEPM Society for Sedimentary Geology
Published: 01 June 2001
PALAIOS (2001) 16 (3): 255–265.
...RICHARD M. STARON; BARBARA S. GRANDSTAFF; WILLIAM B. GALLAGHER; DAVID E. GRANDSTAFF Abstract Rare Earth Element (REE) signatures have been used to test whether mosasaur bones in a basal Hornerstown Formation bonebed (the Main Fossiliferous Layer, or MFL) in New Jersey were reworked from...
Journal Article
Glauconite Composition and Morphology, Shocked Quartz, and the Origin of the Cretaceous(?) Main Fossiliferous Layer (MFL) in Southern New Jersey, U.S.A.
Journal: Journal of Sedimentary Research
Publisher: SEPM Society for Sedimentary Geology
Published: 01 July 2011
Journal of Sedimentary Research (2011) 81 (7): 479–494.
... vertebrates to interpret the genesis of the MFL. Glauconite concentration and maturity steadily increases from latest Cretaceous sediments of the Navesink–New Egypt Formation, through the MFL and into the Paleogene upper Hornerstown Formation, suggesting that marine transgression and decreasing sedimentation...
Journal Article
Latest Cretaceous and Earliest Tertiary Stratigraphy of New Jersey Coastal Plain
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 April 1963
AAPG Bulletin (1963) 47 (4): 643–665.
... are recognized and one of these, the New Egypt Formation, is newly described. The Navesink, Tinton, Hornerstown, and New Egypt Formations lithologically are characterized by a great abundance of the mineral glauconite, which occurs principally as sand-size grains. In contrast, the Redbank Formation is a quartz...
Journal Article
Chemical Composition of Thalassinoides Boxwork Across the Marine K–PG Boundary of Central New Jersey, U.S.A.
Journal: Journal of Sedimentary Research
Publisher: SEPM Society for Sedimentary Geology
Published: 01 December 2016
Journal of Sedimentary Research (2016) 86 (12): 1444–1455.
...Robert J. Horner; Logan A. Wiest; Ilya V. Buynevich; Dennis O. Terry, Jr.; David E. Grandstaff Abstract: Thalassinoides isp. burrow networks filled with green to dark bluish-gray glauconite pellets occur in the Cretaceous to Paleogene Hornerstown Formation and in the uppermost 1–2 m...
Journal Article
Correlation of Paleocene and Eocene Formations and Cretaceous-Paleocene Boundary in New Jersey
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 April 1956
AAPG Bulletin (1956) 40 (4): 722–736.
...Halsey W. Miller, Jr. ABSTRACT The Hornerstown formation is correlated with the Midway stage (Paleocene) of the Gulf Coast. The Vincentown formation is correlated with the Aquia formation (lower Eocene) of Maryland, and the Manasquan formation is correlated with the Claiborne stage (middle Eocene...
Journal Article
Petrology and origin of the lower Tertiary formations of New Jersey
Journal: Journal of Sedimentary Research
Publisher: SEPM Society for Sedimentary Geology
Published: 01 September 1963
Journal of Sedimentary Research (1963) 33 (3): 587–603.
...John K. Adams Abstract The sediments of lower Tertiary age in New Jersey have been divided into 4 formations: the Hornerstown Marl, The Vincentown Sand, the Manasquan Marl, and the Shark River Marl. The writer has recognized 3 of these units in outcrop: the Hornerstown, Vincentown, and Manasquan...
Image
Concentrations of A) Zr, B) Ti, C) K, and D) Fe vs. stratigraphic l...
in Chemical Composition of Thalassinoides Boxwork Across the Marine K–PG Boundary of Central New Jersey, U.S.A.
> Journal of Sedimentary Research
Published: 01 December 2016
Fig. 5.— Concentrations of A) Zr, B) Ti, C) K, and D) Fe vs. stratigraphic level in sediments at Walnridge Farm, New Jersey. Dotted line indicates the New Egypt–Hornerstown Formation boundary. The inferred K–Pg boundary is ∼ 10 cm above the formational boundary. Typical 2σ analytical
Image
Thalassinoides isp. burrows in the upper Navesink and lower Hornerstown fo...
in Chemical Composition of Thalassinoides Boxwork Across the Marine K–PG Boundary of Central New Jersey, U.S.A.
> Journal of Sedimentary Research
Published: 01 December 2016
Fig. 3.— Thalassinoides isp. burrows in the upper Navesink and lower Hornerstown formations at Inversand Quarry, Sewell, NJ (site I in Fig. 1 ). The contact between the chocolate-colored marl of the Navesink Formation and the overlying greenish Hornerstown Formation is at the top pin. Pins
Image
Photographs and Dino-Lite images of trace fossils at Inversand Quarry. A )...
Published: 01 May 2016
Fig. 4.— Photographs and Dino-Lite images of trace fossils at Inversand Quarry. A ) Bedding exposures of Y-junctions characteristic of Thalassinoides in the Hornerstown Formation. B ) Bedding exposure of Y-junction in the underlying Navesink Formation. C ) Bedding exposures of laminated fill
Image
Photographs of measured sections and photomicrographs of glauconite and sho...
in Glauconite Composition and Morphology, Shocked Quartz, and the Origin of the Cretaceous(?) Main Fossiliferous Layer (MFL) in Southern New Jersey, U.S.A.
> Journal of Sedimentary Research
Published: 01 July 2011
. G) Stage 3 glauconite, matrix (M), and pyrite (P) from the Navesink Formation at Sewell, New Jersey. H) Oxidized matrix (Fe) and glauconite from the Hornerstown Formation at Walnridge Farm. I) Close-up of burrow at the Navesink–Hornerstown contact at Sewell. The burrow is filled primarily
Image
Concentrations of A) Zr, B) Ti, C) K, and D) Fe vs. stratigraphic l...
in Chemical Composition of Thalassinoides Boxwork Across the Marine K–PG Boundary of Central New Jersey, U.S.A.
> Journal of Sedimentary Research
Published: 01 December 2016
Fig. 4.— Concentrations of A) Zr, B) Ti, C) K, and D) Fe vs. stratigraphic level in sediments and burrow fills at Inversand, New Jersey. Symbol legend for Figure 4 is in Part A. The Hornerstown–Navesink Formation boundary is indicated by the dashed line. The dotted lines indicate the top
Journal Article
The petrology of the Vincentown Formation [New Jersey]
Journal: Journal of Sedimentary Research
Publisher: SEPM Society for Sedimentary Geology
Published: 01 September 1954
Journal of Sedimentary Research (1954) 24 (3): 212–217.
... formation is the transgressive phase of a marine cycle involving the underlying Hornerstown formation as the initial regressive phase and the overlying Manasquan formation as the final regressive phase. A sub-tropical climate prevailed in the area during the deposition of the Vincentown. The source rocks...
Journal Article
On the last mosasaurs: Late Maastrichtian mosasaurs and the Cretaceous-Paleogene boundary in New Jersey
William B. Gallagher, Kenneth G. Miller, Robert M. Sherrell, James V. Browning, M. Paul Field, Richard K. Olsson, Peter J. Sugarman, Steven Tuorto, Hendra Wahyudi
Publisher: Société Géologique de France
Published: 01 March 2012
Bulletin de la Société Géologique de France (2012) 183 (2): 145–150.
... site in Monmouth County, NJ, the biostratigraphic position of mosasaur specimens ( Halisaurus platyspondylus, Mosasaurus hoffmann ) is related to the occurrence of an iridium excursion of 0.5 ppb (5x background levels) in the basal Hornerstown Formation just above the upper Maastrichtian New Egypt...
Journal Article
An isolated ichthyosaur coracoid from the Maastrichtian of New Jersey
Journal: Canadian Journal of Earth Sciences
Publisher: Canadian Science Publishing
Published: 01 January 1978
Canadian Journal of Earth Sciences (1978) 15 (1): 169–171.
...C. McGowan Abstract An isolated ichthyosaur coracoid from the Hornerstown Formation of New Jersey extends the geological range of the Ichthyosauria at least to the late Maastrichtian. The specimen cannot be referred to any known taxon but is too incomplete to be described as the type of a new...
Image
RELATIVE ABUNDANCE OF GENERA, SPECIES, AND INDIVIDUALS FROM BENTHONIC FORAM...
Published: 01 April 1963
TABLE III. RELATIVE ABUNDANCE OF GENERA, SPECIES, AND INDIVIDUALS FROM BENTHONIC FORAMINIFERAL FAMILIES IN NAVESINK, REDBANK, AND HORNERSTOWN FORMATIONS
Image
Bivariate scatter plots of sediment compositions at Inversand and Walnridge...
in Chemical Composition of Thalassinoides Boxwork Across the Marine K–PG Boundary of Central New Jersey, U.S.A.
> Journal of Sedimentary Research
Published: 01 December 2016
Hornerstown Fm sediment compositions indicating that fill for the Navesink and New Egypt burrows is derived from the overlying Hornerstown Formation and above the MFL at Inversand (Part A). C , D) The filled regions in represent general areas of physical mixing between chemical compositions of Hornerstown
Image
—Map of southern New Jersey showing approximate extent of outcrops of Red B...
in Correlation of Paleocene and Eocene Formations and Cretaceous-Paleocene Boundary in New Jersey
> AAPG Bulletin
Published: 01 April 1956
Fig. 1. —Map of southern New Jersey showing approximate extent of outcrops of Red Bank, Navesink, and Hornerstown formations. “Middle greensand” unit (probably Red Bank formation) indicated where found in pits; patches do not represent outcrops, as none are known. Actual distribution of “middle
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FIGURE 2 —Stratigraphic column of the Inversand Pit. The location of the K-...
in REE Signatures in Vertebrate Fossils from Sewell, NJ: Implications for Location of the K-T Boundary
> PALAIOS
Published: 01 June 2001
FIGURE 2 —Stratigraphic column of the Inversand Pit. The location of the K-T boundary at Inversand has been the subject of continued debate. Some workers place the boundary at the contact between the Navesink and Hornerstown Formation (marked at 3.2 m), others place the boundary within or above
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