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Home > Art, Film & Photography > Geology of Australia: Great Artesian Basin, Geology of Tasmania, Geology of New South Wales, Gondwana, Lachlan Fold Belt, Indo-Australian PL
Geology of Australia: Great Artesian Basin, Geology of Tasmania, Geology of New South Wales, Gondwana, Lachlan Fold Belt, Indo-Australian PL

Geology of Australia: Great Artesian Basin, Geology of Tasmania, Geology of New South Wales, Gondwana, Lachlan Fold Belt, Indo-Australian PL


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About the Book

Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Pages: 29. Chapters: Great Artesian Basin, Geology of Tasmania, Geology of New South Wales, Gondwana, Lachlan Fold Belt, Indo-Australian Plate, Australian Soil Classification, Hunter-Bowen orogeny, Australian Shield, Australasian strewnfield, Centralian Superbasin, Eromanga Basin. Excerpt: Tasmania has a complex geological history, with the world's biggest exposure of diabase, or dolerite. The rock record contains representatives of each period of the Neoproterozoic, Paleozoic, Mesozoic and Cainozoic eras. It is one of the few southern hemisphere areas glaciated during the Pleistocene with glacial landforms in the higher parts. The west coast region hosts significant mineralisation and numerous active and historic mines. Surface geology of Tasmania The earliest geological history is recorded in rocks from over . These older rocks from western Tasmania and King Island were strongly folded and metamorphosed into rocks such as quartzite. After this there are many signs of glaciation from the Cryogenian, as well as the global warming that occurred at the start of the Ediacaran period. An orogeny folded the older Precambrian rocks. In the Cambrian time the Tyennan block forming the south west and central Tasmania, was pushed up and slightly over the land of north west Tasmania, the Tyennan Orogeny. Then there were volcanic action and sediments from the Cambrian and Ordovician. The large ore deposits were formed on the West Coast. The north east of Tasmania began to form as part of the Lachlan Orogen with turbidity flows of mud and sand on to the ocean floor. In the Devonian the Taberabban Orogeny caused more folding, and intrusion of granite on the west and east coasts, and probably joined the east of Tasmania to the west. In the Permian period, conditions were again glacial and the Tasmania basin formed, with low sea levels in the Triassic....


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Product Details
  • ISBN-13: 9781156837504
  • Publisher: Books LLC, Wiki Series
  • Publisher Imprint: Books LLC, Wiki Series
  • Height: 246 mm
  • No of Pages: 30
  • Spine Width: 2 mm
  • Weight: 73 gr
  • ISBN-10: 1156837502
  • Publisher Date: 06 Sep 2011
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Sub Title: Great Artesian Basin, Geology of Tasmania, Geology of New South Wales, Gondwana, Lachlan Fold Belt, Indo-Australian PL
  • Width: 189 mm


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