2 edition of Sediments of Shark Bay and Macleod Basin, western Australia found in the catalog.
Sediments of Shark Bay and Macleod Basin, western Australia
Brian W. Logan
by Sedimentology Research Group, Dept. of Geology, University of Western Australia in Perth
Written in English
Includes bibliographical references (p. 218-229).
|Other titles||Field seminar handbook|
|Statement||by Brian Logan and R.G. Brown.|
|Contributions||Brown, R. G.|
|The Physical Object|
|Pagination||229 p. :|
|Number of Pages||229|
Maps were prepared using high resolution (50 cm per pixel) Shark Bay orthophotographs from the Department of Environment and Conservation (DEC) and from Landgate (Perth, WA, Australia). In addition, a set of Shark Bay aerial‐photographs (1: ) from Landgate was interpreted using stereoscopy equipment to support map construction. Shark Bay & Lake MacLeod. Shark Bay Stromatolites. Lake MacLeod. an analogue to Holocene evaporites of the United Arab Emirates and Lake MacLeod of Western Australia: American Association of Petroleum and P.M. Harris, , Hydrocarbon occurrence in Guadalupian sediments, the Permian basin, West Texas and New Mexico. Am. Assoc.
Lake Macleod is a lake that as a result of evaporation of influxing of sea water through the Pleistocene country rock lies below sea level. It periodically is flooded by freshwater from monsoonal rains. It is situated just north of Shark Bay and Carnarvon, Western Australia. PDF | On Jan 1, , C.B. Jonhnson and others published Gold-bearing Palaeochannel Sediments at Gidgi, Western Australia | Find, read and cite all the research you need on ResearchGate.
SALMONID FISHES FROM MIO-PLIOCENE LAKE SEDIMENTS IN THE WESTERN SNAKE RIVER PLAIN AND THE GREAT BASIN By Ralph F. Stearley and Gerald R. Smith. Miscellaneous Publication , No. 1; Museum of Zoology, University of Michigan. Ann Arbor, MI. This book is soft-bound in light blue wrappers, with black and color pictorial printing to the upper Seller Rating: % positive. Carnarvon Basin (Figure 1), which corresponds almost exactly to the western half of Shortridge's 'Centraldistrict'(Shortridge, ). Virtually all the mammal records from the study area prior to AD are from the Shark Bay islands and Peron Peninsula. These are reviewed in Ride et al. (). The earliest island records were.
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Sediments of Shark Bay and Macleod Basin, western Australia [Brian W Logan] on *FREE* shipping on qualifying : Brian W Logan. Evolution and diagenesis of Quaternary carbonate sequences, Shark Bay, Western Australia Brian W.
Logan American Association of Petroleum Geologists, - Carbonate rocks - pages. Shark Bay is an sq. km shallow marine embayment on the western coast of Western Australia. The waters exhibit a well established salinity gradient from oceanic to hypersaline.
The chemical assemblage of sediment hydrocarbons along the salinity gradient may be classified into two distinct chemogeographic by: Logan BW, Hagan GM () Calcrete deposits and quaternary sediments of Hamelin Basin, Shark Bay, Western Australia.
In: Logan BW et al (eds) Carbonate sedimentation and environments, Shark Bay, Western Australia, Mem American Association of Petroleum Geologists, Tulsa Google ScholarAuthor: Andrew D. Short. ‘Shark Bay Depres sion’, a central p art termed the ‘MacLeod Graben’, and a northern part termed the ‘Dingo Syncli ne’.
Mai n geographic n ames are also s hown. Unusual occurrences of large blocks on top of cliffs overlooking the sea have been interpreted as debris scattered by the force of so-called mega-tsunamis that struck the Western Australian coast up to years ago.
Several of these deposits have been discovered at Shark Bay, Barrow Island, Legendre Island and along the Kimberley coast. coastal playas of Lake Macleod and Shark Bay.
The northern Perth Basin contains a distinct coastal plain with signiﬁ cant heavy mineral sand deposits at the foot of. Shark Bay Marine Park is compartmented into three major embayments: Freycinet, L'Haridon Bight and Hamelin Pool.
Freycinet embayment in the western Shark Bay maintains the best connection with northerly oceanic waters so that despite the high evaporation, salinity is metahaline (40–56; Logan and Cebulski, ).
Hamelin Pool, the easterly. The geology of Western Australia spans billion years of Earth's history — from the oldest dated zircon mineral grains at Jack Hills and ancient million-year-old Archean gneiss in the Narryer Terrane, to recent sediments forming right now on the Swan Coastal Plain around Perth.
The Carnarvon Basin study area covers 75 km2 on Australia's western coast. It is centred on Shark Bay, and extends northwards from the Murchison River to the Minilya River, and eastwards to °30'E (beyond Gascoyne Junction) (Figure 1).
Its physicalenvironments are detailedbyWyrwoll, Courtney and Sandercock () and Wyrwoll. Shark Bay, Western Australia: in Logan et al., Carbonate Sedimentation and Environments, Shark Bay, Western Australia: American Association of Petroleum Geologists Mem p.
Shark Bay (Malgana: Gutharraguda, "two waters") is a World Heritage Site in the Gascoyne region of Western 23,square-kilometre (8, sq mi) area is located approximately kilometres ( mi) north of Perth, on the westernmost point of the Australian continent.
UNESCO's official listing of Shark Bay as a World Heritage Site reads. Holocene Intertidal Stromatolites and other Carbonates of Shark Bay, Western Australia Photographs of some of the best known Holocene intertidal stomatolite heads in the world.
Most photos were taken by Christopher Kendall on various field trips to Shark Bay and Lake MacLeod lead by Brian Logan. Logan BW () Inventory of diagenesis in Holocene-Recent carbonate sediments, Shark Bay, Western Australia. Am Assoc Petrol Geol Mem – Google Scholar Logan BW, Brown RG () Field seminar handbook of Shark Bay and Macleod Basin, Western Australia.
Get this from a library. Environments, foraminiferal facies and sediments of Shark Bay, Western Australia. [Brian W Logan]. Located on the west coast of Australia (at 25° 30′–26° 30′S & ° 30′ –° 30′E) Shark Bay is a World Heritage site with Hamelin Pool the most notable embayment renowned for its extraordinary bacterial deposits, sea grasses and extensive coquina n Pool is a U-shaped embayment semi-closed to the north by a large seagrass bank cut by tidal channels (Logan and.
Coastal deposits along the western coastal margin of Australia, a region of relative tectonic stability, record Plio-Pleistocene events and processes affecting the inner shelf and adjacent hinterland. Tectonic deformation of these deposits is more apparent in the Carnarvon Basin, and rather less so in the Perth Basin.
Basin biogeographic region. The reduced island diversity is presumably due to a combination of lesser sampling effort and'drop out'extinctions following drowning of the continental shelf and severance of the island around 6S00 years ago.
Key words: Shark Bay World Heritage Property, herpetofauna, reptiles, 'drop out'extinction, continental shelf. The streamed video chalk board lecture below explains the ideal Vail et al sequence, and considers this in terms of the component systems tracts, and their gross geometries as products of changes in relative sea level and the evolving accommodation' space.
You are introduced to sea level and base level, sequence, concepts of sequence stratigraphy from the perspective of evolving sediment.
The Geology of Shark Bay. Geological Survey of Western Australia(). Playford P. Stromatolite research in Western Australia. Royal Soc. West. Austra 13–20 (). McNamara K. Stromatolties. 87 (Western Australian Museum, ).
8. RECENT MODELS FOR INTERPRETING STROMATOLITE ENVIRONMENTS Chapter MODERN ALGAL STROMATOLITES AT HAMELIN POOL, A HYPERSALINE BARRED BASIN IN SHARK BAY, WESTERN AUSTRALIA P.E. Playford and A.E.
Cockbain INTRODUCTION Algal stromatolites are forming today over wide areas of the sublittoral platform and adjacent intertidal zone fringing Hamelin Pool, a hyperialine barred basin .A wonderland of world-class natural attractions, the Shark Bay World Heritage Area was the first location in Western Australia to receive UNESCO status in The area meets four of the ten required natural criteria and remains one of only a handful of places in the world to achieve this high criteria status level.Shark Bay & Lake MacLeod.
Shark Bay Stromatolites. Lake MacLeod. Saudi Arabian Outcrops. Tepee Structures. sedimentary sections lying east of the Caledonides Mountains of Ireland in geological localities that mirror the sediments of the western Appalachians.
Shark Bay, Western Australia - Holocene Carb onates.