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  2. Microplate - Wikipedia

    en.wikipedia.org/wiki/Microplate

    The well position is also standardized, but only for 96- , 384-, and 1536-well plates. These are generally well followed by manufacturers: Well Positions [16] [17] 96-well plates have a 9 mm well-to-well spacing, 384-wells a 4.5 mm spacing, and 1536-wells a 2.25 mm spacing. A notable characteristic is that the well array is symmetrical when the ...

  3. File:Tectonic plates boundaries World map Wt 180degE centered ...

    en.wikipedia.org/wiki/File:Tectonic_plates...

    This map was improved or created by the Wikigraphists of the Graphic Lab (fr). You can propose images to clean up, improve, create or translate as well. This SVG file contains embedded text that can be translated into your language, using any capable SVG editor, text editor or the SVG Translate tool .

  4. List of tectonic plates - Wikipedia

    en.wikipedia.org/wiki/List_of_tectonic_plates

    These plates are often grouped with an adjacent principal plate on a tectonic plate world map. For purposes of this list, a microplate is any plate with an area less than 1 million km 2 . Some models identify more minor plates within current orogens (events that lead to a large structural deformation of Earth's lithosphere ) like the Apulian ...

  5. File:96-Well plate.svg - Wikipedia

    en.wikipedia.org/wiki/File:96-Well_plate.svg

    Here, I redesigned the 96-well plate figure working from an overlay of a 96-well plate manufacturer technical drawing, and the official SLAS/ANSI 96-well plate size standards. Designed in Inkscape. 16:42, 29 May 2020: 672 × 452 (70 KB) FlowerFaerie087: Minor edit for consistent, smooth image: 15:43, 29 May 2020: 672 × 452 (76 KB) FlowerFaerie087

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  7. List of tectonic plate interactions - Wikipedia

    en.wikipedia.org/wiki/List_of_tectonic_plate...

    Obduction zones occurs when the continental plate is pushed under the oceanic plate, but this is unusual as the relative densities of the tectonic plates favours subduction of the oceanic plate. This causes the oceanic plate to buckle and usually results in a new mid-ocean ridge forming and turning the obduction into subduction. [citation needed]

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