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Ironshore Formation

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Journal Article
Journal: PALAIOS
Published: 01 June 2000
PALAIOS (2000) 15 (3): 212–224.
...DAVID J. HILLS; BRIAN JONES Abstract Rhodoliths from the Late Pleistocene Ironshore Formation in the Crystal Harbour area on the western part of Grand Cayman, which are up to 14 cm long, are characterized by thick cortices that were constructed around nucleii formed primarily of coral or bivalve...
FIGURES | View All (9)
Journal Article
Published: 01 March 1999
Journal of Sedimentary Research (1999) 69 (2): 317–327.
...Jennifer Vezina; Brian Jones; Derek Ford Abstract The Ironshore Formation (up to 19 m thick) in the Rogers Wreck Point area of Grand Cayman is divided into the unconformity-bounded units A, B, C, and D. The unconformities are highlighted by caliches and/or terra rossa. Th/U dates from aragonitic...
Journal Article
Published: 01 April 1990
Canadian Journal of Earth Sciences (1990) 27 (4): 525–532.
...Brian Jones Abstract Pleistocene limestones of the Ironshore Formation, deposited approximately 125 000 years ago, contain stellate tunicate spicules that are morphologically similar to those of the modern Trididemnum strigosum Kott, 1980 from Australia. The aragonite spicules, up to 0.1 mm...
Journal Article
Journal: PALAIOS
Published: 01 September 1989
PALAIOS (1989) 4 (4): 343–355.
Journal Article
Published: 01 July 1988
Journal of Paleontology (1988) 62 (4): 495–505.
Journal Article
Published: 01 June 1988
Bulletin of Canadian Petroleum Geology (1988) 36 (2): 191–201.
...Brian Jones ABSTRACT Study of a caliche unit in the Pleistocene Ironshore Formation on Cayman Brac, British West Indies, demonstrates that plant roots and their associated micro-organisms played an important role in its diagenesis. The root borings, which are up to 25 cm in diameter and at least 4...
Journal Article
Journal: PALAIOS
Published: 01 February 1988
PALAIOS (1988) 3 (1): 3–21.
...Brian Jones; S. George Pemberton RESEARCH REPORTS 3 Lithophaga Borings and their Influence on the Diagenesis of Corals in the Pleistocene Ironshore Formation of Grand Cayman Island, British West Indies BRIAN JONES and S. GEORGE PEMBERTON Department of Geology, University of Alberta, Edmonton...
Image
FIGURE 3 —Rhodoliths from <span class="search-highlight">Ironshore</span> <span class="search-highlight">Formation</span> at Crystal Harbour, Grand Cay...
Published: 01 June 2000
FIGURE 3 —Rhodoliths from Ironshore Formation at Crystal Harbour, Grand Cayman. (A) Large spherical rhodolith with smooth exterior. (B) Discoidal rhodolith with globular surface. (C) Cross section through rhodolith formed by red algae growing around a bivalve shell. (D) Concentric laminae growth
Journal Article
Published: 01 March 2003
Journal of Sedimentary Research (2003) 73 (2): 187–205.
...Brian Jones; Robert W. Luth Abstract On the Cayman Islands, the Tertiary Bluff Group (Brac Formation, Cayman Formation, Pedro Castle Formation) is onlapped and overlain by the Pleistocene Ironshore Formation. On Grand Cayman, the Brac Formation and Cayman Formation are formed of finely crystalline...
FIGURES | View All (18)
Journal Article
Published: 01 November 1989
Canadian Journal of Earth Sciences (1989) 26 (11): 2204–2213.
...Brian Jones Abstract Phytokarst is spectacularly developed on the hard, finely crystalline dolostones of the Oligocene–Miocene Bluff Formation and to a lesser extent on the soft limestones of the Pleistocene Ironshore Formation on Grand Cayman. The black weathered surfaces, which are a reflection...
Image
Distribution of Cayman <span class="search-highlight">Formation</span>, Pedro Castle <span class="search-highlight">Formation</span>, and <span class="search-highlight">Ironshore</span> For...
Published: 01 November 2003
Figure 3 Distribution of Cayman Formation, Pedro Castle Formation, and Ironshore Formation at selected localities on Grand Cayman. Note different distribution styles of hard, low-porosity dolostones and friable, high-porosity dolostones in Cayman Formation. Inset map shows location of wells
Journal Article
Published: 01 June 1984
Bulletin of Canadian Petroleum Geology (1984) 32 (2): 190–200.
...Brian Jones; Q. H. Goodbody ABSTRACT Ooids in the Pleistocene Ironshore Formation of Grand Cayman Island generally have large nuclei and a thin cortex. The morphology, composition and texture of the nuclei suggest that they originated as pellets, proably from the burrowing shrimp Callianassa...
Journal Article
Published: 01 November 1989
Journal of Sedimentary Research (1989) 59 (6): 1002–1007.
...Brian Jones; Cheryl A. Squair Abstract Spherical to elliptical peloids, averaging 80 mu m in length, occur inside plant rootlets that penetrate limestones of the Pleistocene Ironshore Formation on Grand Cayman. The peloids, which are associated with desiccated fragments of mites, are formed...
Journal Article
Published: 01 May 1988
Journal of Sedimentary Research (1988) 58 (3): 457–467.
...Brian Jones; Kwok-Choi Ng Abstract Rhizoliths from the Pleistocene Ironshore Formation are formed of a brown micrite core surrounded by sediment that is well cemented with 1) calcite rhomb chains, 2) isolated calcite rhombs, 3) calcified spherical bodies, 4) Types I and II calcified epilithic...
Image
Distribution of dolostones, limestones, and dominant biota in Bluff Group a...
Published: 01 November 2003
Figure 2 Distribution of dolostones, limestones, and dominant biota in Bluff Group and Ironshore Formation on Grand Cayman (modified from Jones 1994 ).
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Location maps.  A)  Location of Grand Cayman in Caribbean Sea.  B)  Geologi...
Published: 01 July 2007
Figure 1 Location maps. A) Location of Grand Cayman in Caribbean Sea. B) Geological map of Grand Cayman showing distribution of Cayman Formation, Pedro Castle Formation, and Ironshore Formation (modified from Jones 1994 ) and locations of wells BAC#1 and DBH#1.
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Schematic cross section from Paul Bodden Quarry (PBQ) to Hell ( Fig. 1A ) s...
Published: 01 March 2003
Figure 8 Schematic cross section from Paul Bodden Quarry (PBQ) to Hell ( Fig. 1A ) showing stratigraphic relationships between the Cayman Formation, Pedro Castle Formation, and Ironshore Formation. Succession in well SH#3 shows distribution of limestone and dolostone through Cayman Formation
Image
A)  Map showing surface geology of Grand Cayman, location of Pedro Castle Q...
Published: 01 July 2002
Figure 1 A) Map showing surface geology of Grand Cayman, location of Pedro Castle Quarry, and location of Sewerage Works site. B) Map of Sewerage Works site showing locations of wells SHT#2, STW, SHT#5, and SHT#3. C) Distribution of the Ironshore Formation (IF), Pedro Castle Formation (PCF
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FIGURE 1 —Maps showing geological and paleogeographical setting of rhodolit...
Published: 01 June 2000
the Sangamon highstand, ∼125,000 years, when carbonate sediments of the Ironshore Formation were accumulating. From Jones and Hunter (1990)
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FIGURE 4 —Size and morphology of rhodoliths collected from the <span class="search-highlight">Ironshore</span> Fo...
Published: 01 June 2000
FIGURE 4 —Size and morphology of rhodoliths collected from the Ironshore Formation at Crystal Harbour, Grand Cayman. (A) Zingg graph for rhodoliths from localities W, NS, and SS. Note that most rhodoliths are spheroidal. (B) Zingg graph showing that there is no relationship between shape and mean