type-plate - ορισμός. Τι είναι το type-plate
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Τι (ποιος) είναι type-plate - ορισμός

TRANSITION BETWEEN OCEANIC AND CONTINENTAL LITHOSPHERE THAT IS NOT AN ACTIVE PLATE MARGIN
Passive plate margin; Atlantic-type margin
  • Passive continental margin
  • Rifting-to-spreading transition

Microplate         
  • [[Liquid handling robot]] for 96 wells
  • A commercial microplate washer
FLAT PLATE WITH MULTIPLE "WELLS" USED AS SMALL TEST TUBES
Microtiter plates; 96 well plate; Microtitre plate; Microwell plate; 96-well plate; Micro-plate; Microtiter plate
A microplate, also known as a microtiter plate (Microtiter is a registered trademark in the United States, therefore it should not be used generically without attribution), microwell plate or multiwell, is a flat plate with multiple "wells" used as small test tubes. The microplate has become a standard tool in analytical research and clinical diagnostic testing laboratories.
Diamond plate         
  • Part of a diamond plate
TEXTURED METAL STOCK WITH A REGULAR PATTERN OF RAISED DIAMONDS OR LINES ON ONE SIDE
Checkerplate; Checker plate; Durbar floor plate; Durbar plate; Diamond plate
Diamond plate, also known as checker plate and tread plate, is a type of metal stock with a regular pattern of raised diamonds or lines on one side, with the reverse side being featureless. Diamond plate is usually steel, stainless steel or aluminum.
Tread plate         
  • Part of a diamond plate
TEXTURED METAL STOCK WITH A REGULAR PATTERN OF RAISED DIAMONDS OR LINES ON ONE SIDE
Checkerplate; Checker plate; Durbar floor plate; Durbar plate; Diamond plate
Tread plate, also known as checker plate and diamond plate, is a type of metal stock with a regular pattern or lines on one side for slip resistance. The most common alloy used for aluminum tread plate is 6061, although 5086-H34 and 3003-H231 are also used.

Βικιπαίδεια

Passive margin

A passive margin is the transition between oceanic and continental lithosphere that is not an active plate margin. A passive margin forms by sedimentation above an ancient rift, now marked by transitional lithosphere. Continental rifting forms new ocean basins. Eventually the continental rift forms a mid-ocean ridge and the locus of extension moves away from the continent-ocean boundary. The transition between the continental and oceanic lithosphere that was originally formed by rifting is known as a passive margin.