Oolite walkthrough1/25/2024 See Coluber (& Deeper Space), CB (& CRR), Vimana & Z-GrOovY MiLHUD below for examples.Ĥ) A number of HUDS have special features Most of these do not have a small variant, so you will find that your small ship defaults to the Vanilla game HUD!Ģ) The number of MFDs varies with the HUD (from 0 to 15)!ģ) HUD designers often include icons for their favourite oxp equipments. It will then help manage most others you download.ġ) The game specifies 2 types of HUD: small (for the Adder, the Cobra Mk.1, etc) and regular. The easiest way into all this is probably using HUDSelector which comes with 3 more HUDs to try out (extra-large, large & small). HUDs not shown here: Note also that some HUDs are not shown here: Killer Wolf's Dynamic HUD, Cyan HUD, Clear HUD, etc. Ships with custom HUDs: Note also that some ships come with their own HUD versions! Eg.: Coluber Racers - Blue, Red, Yellowbelly & Black also Isis Interstellar ships, all of Simon B's ships in Neolite-Wolfies and some of his Waka series, some of Wolfwood's ships such as his Asp Explorer (Oolite), etc. The most striking versions here include the Coluber, Dangerous & Vimana HUDs. This happened with the release of Oolite v.1.79 in 2013/4. There was a quantum leap under Cim's tenure as lead designer, when it was made easier to code new HUDs and the range of possibilities was greatly increased. A HUD also has the advantage that the pilot's eyes do not need to refocus to view the outside after looking at the optically nearer instruments First developed in the 1940s for military aircraft (from Wikipedia).Īs the newer versions of Oolite have allowed more flexibility with modifying HUD elements since the early days of Oolite v.1.20 in 2004! From the halcyon days of Aegidian's Mega-Walnut dashboard (for the Fer-de-Lance), the HUD designers have risen to the challenge. The origin of the name stems from a pilot being able to view information with the head positioned "up" and looking forward, instead of angled down looking at lower instruments. A HUD is a Heads-Up Display: a transparent display that presents data without requiring users to look away from their usual viewpoints. and Ulmer-Scholle, D.Images are below their captions. James, N.P., 1984, Shallowing-upward sequences in carbonates, in Walker, R.G., ed., Facies Models: Geological Association of Canada, Geoscience Canada, Reprint Series 1, p. 1-38.įolk, R.L., 1962, Spectral subdivision of limestone types, in Ham, W.E., ed., Classification of carbonate Rocks-A Symposium: American Association of Petroleum Geologists Memoir 1, p. 730-781.įolk, R.L., 1959, Practical petrographic classification of limestones: American Association of Petroleum Geologists Bulletin, v. 108-121.Įmbry, AF, and Klovan, JE, 1971, A Late Devonian reef tract on Northeastern Banks Island, NWT: Canadian Petroleum Geology Bulletin, v. (ed.), Classification of carbonate Rocks: American Association of Petroleum Geologists Memoir, p. J., 1962, Classification of carbonate Rocks according to depositional texture. ![]() Terms such as bafflestone, bindstone, and framestone are useful in concept but are extremely difficult to apply to ancient limestones where diagenesis and sample size limit ones ability to assess an organisms function.ĭunham, R. Embry and Klovan to more graphically reflect the role that the organisms performed during deposition also modified the boundstone classification of Dunham. In their revised scheme, a wackestone in which the grains are greater than 2mm in size is termed a floatstone and a coarse grainstone is called a rudstone.īoth terms are extremely useful in description of limestones. Embry has modified Dunham's classification and Klovan (1971) to include coarse grained carbonates (above figure). ![]() The wide range of percentage of mud matrix that a carbonate may have and still be termed a packstone by Dunham sometimes reduces the utility of this classification. Moreover, a Rock containing little matrix is termed a sparite by Folk and a grainstone or packstone by Dunham. If one compares the two classifications, a Rock rich in carbonate mud is termed a micrite by Folk and a mudstone or wackestone by Dunham. If the sediment is mud supported but contains more than 10 percent grains, then it is known as a wackestone, and if it contains less than 10 percent grains and is mud supported, it is known as a mudstone. If the carbonate is grain supported but contains a small percentage of mud, then it is known as a packstone. For example, if the grains of a limestone are touching one another and the sediment contains no mud, then the sediment is called a grainstone. ![]() For this reason, his scheme may be better suited for Rock descriptions that employ a hand lens or binocular microscope. In contrast, Dunham's classification (figures above) and its modification by Embry and Klovan (1971) and James (1984) deals with depositional texture.
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