![]() Geological Society of London, Special Publication, 46, ix–xxv. Phanerozoic ironstones: an introduction and review. Journal of Sedimentary Research, 55: 171–183. Submarine hydrothermal weathering, global eustasy, and carbonate polymorphism in phanerozoic marine oolites. Nearshore oolite formation in a modern temperate-region marl lake. American Association of Petroleum Geologists Bulletin. Journal of Sedimentary Petrology, 63: 974–982. Numerical modeling of ooid size and the problem of Neoproterozoic giant ooids. Sumner, D.A., and Grotzinger, J.P., 1993. Aragonite oöids: experimental precipitation from seawater in the presence of humic acid. Paleogeography, Paleoclimatology, Paleoecology, 144: 3–19. Secular oscillations in the carbonate mineralogy of reef-building and sediment-producing organisms driven by tectonically forced shifts in seawater chemistry. Quarterly Journal of the Geological Society of London, 35 (Proceedings), 56–95. On the structure and origin of limestones. Palaeontographica Americana, 54: 272–281. Recognition criteria for calcitized skeletal and non-skeletal aragonites. An oscillating trend in phanerozoic non-skeletal carbonate mineralogy. New interpretations of Great Salt Lake ooids and of ancient non-skeletal carbonate mineralogy. A rock consisting of fine grains of carbonate of lime 1.4 Class Sedimentary Rocks 1.4. Holocene lacusterine ooids from Pyramid Lake, Nevada. Oolite is a sedimentary rock formed from ooids, spherical grains which are composed of concentric layers of calcite 1.2 History 1.2.1 Origin Unknown 1.2.2 Discoverer Unknown 1.3 Etymology From oo- + -lite, after German Oolit. Developments in Sedimentology, Volume 55, Elsevier. Carbonate Reservoirs, Porosity Evolution and Diagenesis in a Sequence Stratigraphic Framework. Journal of Sedimentary Petrology, 45: 285–291. High magnesium calcite ooids from the Great Barrier Reef. A Manual of Elementary Geology, 4th edn, New York: D. Distribution and ultrastructure of Holocene ooids from the Persian Gulf. Journal of Sedimentary Petrology, 49: 1269–1278. Zeitschrift Der Deutschen Geologische Gesellschaft, 60: 68–125. Oolith und Stromatolith im norddeutschen Buntsandstein. AAPG Studies in Geology, Volume 35, Tulsa: American Association of Petroleum Geologists. Mississippian Oolites and Modern Analogs. ![]() Journal of Sedimentary Research, 64: 101–114. Paleogeographic and paleoclimatic controls on ooid mineralogy of the Smackover Formation, Mississippi salt basin: implications for Late Jurassic seawater composition. Journal of Sedimentary Petrology, 53: 193–208. Formation and infilling of pits of marine ooid surfaces. Organic matter, putative nannobacteria and the formation of ooids and hardgrounds. Synthesis and possible mechanisms of formation of radial carbonate ooids. Springer-Verlag.įerguson, J., Bubela, B., and Davies, P.J., 1978. Schweizerbart'sche Verlagsbuchhandlung.įlügel, E., 1982. Contributions to Sedimentology, Volume 7, Stuttgart: E. Radial aragonite ooids, Lizard Island, Great Barrier Reef. Journal of Sedimentary Research, 71: 423–429.ĭavies, P.J., Bubela, B., and Ferguson, J., 1978. Recent freshwater ooids and oncoids from western Lake Geneva (Switzerland): indications of a common organically mediated origin. Bacterially induced lithification of microbial mats. Paris: Masson.Ĭhafetz, H.S., and Buczynski, C., 1992. Les Roches Sédimentaires De France, Roches Carbonatées. Developments in Sedimentology, Volume 12, Elsevier.Ĭayeux, L., 1935. ![]() Carbonate Sediments and Their Diagenesis. And in the darkness between the stars, an old enemy lurks, fearless, perhaps waiting for order to collapse entirely.Bathurst, R.C.G., 1975. The mercenaries they hire for a few credits a kill are too few, too unreliable to do so either. The Cooperative's police force, concentrated near a few influential planets, can no longer maintain order. The trade ships that once safely travelled between planets now have to be well armed and escorted to fend off pirate attacks, from small-time criminals desperate for their next meal, to powerful robber barons extracting tithes from everyone who passes through their space. The two thousand star systems of the Cooperative once enjoyed a golden age of peace and prosperity, and perhaps the wealthiest of them can still pretend to. Perhaps one day, everyone might know your name. You've got a ship, some weapons, and enough spare cash to get started - and one day, you might get the fame, wealth or glory you want. Among the seven trillion people who are - at least officially - Cooperative citizens, you are nobody. ![]()
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