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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 ...
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
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 ...
Where the plates meet, their relative motion determines the type of plate boundary (or fault): convergent, divergent, or transform. The relative movement of the plates typically ranges from zero to 10 cm annually. Faults tend to be geologically active, experiencing earthquakes, volcanic activity, mountain-building, and oceanic trench formation.
The Pacific plate is moving the fastest at 95 mm/yr NE, then the Cocos plate moving relatively N-NW 67 mm/yr, and 40 mm/yr E –NE for the Nazca plate. [2] Differing border velocities that detect the rate of spreading as well as the lack of/slowing of spreading are also considered as well.
I designed the figure from an overlay of a 384-well plate manufacturer technical drawing. Designed in Inkscape. The Inkscape "Tiled clone" tool where the percentage row/column shift was calculated by (well spacing/well width-1.00)*100 (in this case, 12.5%), was essential to producing regularly spaced wells.
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In this area, the main sedimentological controls for the accumulation of gas hydrates are the sand-rich areas of the trough (Collett, 2002). Well coring indicates the presence of at least three gas hydrate zones. Krason, 1994, estimated that there are 0.42 to 4.2×10 12 cubic meters of methane within the gas hydrates. Seismically, the high ...