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By Arnold Henry Savage Landor

Arnold Henry Savage Landor' memoirs of his excursion to unknown South the United States and his come upon with the local Bororo Indians. initially written in volumes, this publication contains illustrations, maps, plates and pictures

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Hayes. Evolution of the Tasman Sea reappraisal. Earth Planetary Science Letters, 36, 77-84, 1977. S. W. McMullan. Australian long-wavelength magnetic anomalies. BMR Journal of Australian Geology & Geophysics, 9, 297-302, 1985. 1. M. Hunt. Crustal structure across the Tasman Sea. New Zealand Journal of Geology and Geophysics, 14, 39-45, 1971. Zhou, B. J. Mills. Multiple dyke emplacement in the Wonominta Block, western New South Wales, Australia and its tectonic significance in relation to Tasman Line.

P. A review of the Precambrian and lower Palaeozoic. tectonics of South Australia. Royal Society of South Australia, Transactions, 94, 193-221, 1970. J. Precambrian. F. L. , Geology and Mineral Resources of Tasmania. Geological Society ofAustralia, Special Publication, 15, 5-46, 1989. , ed. , 1984. 1. Tectonic-climatic supercycle in the billionyear plate-tectonic eon: Permian Pangean icehouse alternates with Cretaceous dispersed continents greenhouse. Sedimentary Geology, 68, 1-16, 1990. G. McA.

H. ,P. Project 257, 435-443, 1990. BROKENHILL-SYDNEY-TASMAN SEA TRANSECfEASTERN AUSTRALIA ATTACHMENT LITHOLOGIC DESCRIPTIONS Broken Hill - Sydney - Tasman Sea Transect Legend Adelaide Fold Belt (miogeoclinal, foreland fold & thrust belt) E1 Cambrian Intrusions Basic, ultrabasic intrusions, some date in the range 500-565 Ma, others age unknown, example is Little Broken Hill Gabbro; this igneous activity probably related to the development of the active plate margin in the east. Early Cambrian E 1 pi Acacia Downs Formation Quartzite, shale, siltstone.

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