7/14/2023 0 Comments Endview planeExtremitySymbolByEndCutType Draw Indicates stiffener end symbol is (A value of 2 results in a placed symbol twiceĪs big.) ChapterName The name of the chapter containingĮxtremity symbols within the Drawing Symbol Structure Catalog.ĭefaultExtremitySymbol The default symbol used to represent the end of a stiffener ReferenceScale Scale factor to apply to the symbol as drawn. Of the stiffener, taking into account the ReferenceScale and the Symbol placed at an extremity may not exceed 45% of the total length There is enough room to draw the extremity symbols without overlap. No is the default (arrowheads are not drawn.) MinimumLengthRatio A percentage of the length of the stiffener used to determine if The following shows a stiffener in TopView FarSideĮxtremitySymbol Draw Indicate Yes to draw arrowheads at the extremities. SymbolLocation The location on the line representation of the plate where the (Refer to PRM file.) SymbolName The symbol name to draw. ![]() ChapterName The name of the chapter containingįlangeOrientation symbols within the Drawing Symbol Structure Catalog. Default is 15.0.įor stiffeners: TopView, SideView, EndViewįlangeOrientationSymbol Draw To draw a flange orientation symbol at the ends of a stiffener.ĭefault is Yes. No indicates the object will not be extracted. Towards the bottom of the file under StructureObjects. In the sample XML file, generative view style parameters for View styles, how to set view style parameters or more generally onĪdministering generative view styles, see the Generative Draftingįor graphic replacement for reference plane systems, ![]() Licenses including one for Generative Drafting are required.įor information on how to create views using generative Planes that will be used for a given project are defined in an XML file OS/resources/standard/generativeparameters.Ĭustomizing parameters in this file affects the appearance of your The sample XML file provided with this application is Photomicrograph of wollastonite in plane and crossed polarized light showing elongated crystals having parallel extinction.How to generate graphic replacement for stiffeners. Wollastonite typically has no color, and has distinct splintery cleavage in an end view. Photomicrograph of wollastonite in plane light (roll over image). ![]() Wollastonite has parallel extinction and has two good cleavages that intersect at an angle of 84º. Photomicrograph of wollastonite in plane and crossed polarized light (roll over image). Sarah Martell (AC '06), Carolyn Tewksbury ('07), Jessica Chang ('17) (1963) Rock-Forming Minerals, Chain Silicates, p. Associated minerals include calcite, and grossular in hornfels, tremolite, epidote group members, diopside, and other Ca-Mg silicates.ĭeer, W.A., Howie, R.A., Zussman, J. Occurs commonly as a product of contact and/or regional metamorphism in limestone and dolomite. One perfect cleavage and two good cleavages producing splintery cleavage fragments. First order interference color yellow-orange. Wollastonite resembles tremolite and pectolite, but both have a higher birefringence.Įlongate crystals display parallel extinction.Ĭolorless to grey in thin sectionwith moderate to moderatly high relief. This can be higher for Fe-bearing samples.Ĭleavage fragments are length slow or length fast depending on orientation due to Y being parallel to fiber length. Angles of cleavage: 84.5 degrees, and 70 degrees.Ĭolorless, white, greyish, often with yellowish or brownish tint. Usually pure, but Mn and Fe2+ can substitute for Ca.Ĭolumnar and fibrous elongate grains, often with twinning
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