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A microplate typically has 6, 12, 24, 48, 96, 384 or 1536 sample wells arranged in a 2:3 rectangular matrix. Some microplates have been manufactured with 3456 or 9600 wells, and an "array tape" product has been developed that provides a continuous strip of microplates embossed on a flexible plastic tape. [2]
Matrix ChIP: This is a microplate-based ChIP assay with increased throughput and a simplified procedure. All steps are done in microplate wells without sample transfers, enabling potential for automation. It enables 96 ChIP assays for histone and various DNA-bound proteins in a single day. [23]
Plate readers, also known as microplate readers or microplate photometers, are instruments which are used to detect biological, chemical or physical events of samples in microtiter plates. They are widely used in research, drug discovery , [ 1 ] bioassay validation, quality control and manufacturing processes in the pharmaceutical and ...
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, Explorer, Gorda, and Philippine Mobile Belt plates. [ 2 ]
The Gonâve microplate, showing the fault zones that bound it. The Gonâve microplate forms part of the boundary between the North American plate and the Caribbean plate.It is bounded to the west by the Mid-Cayman Rise spreading center, to the north by the Septentrional-Oriente fault zone and to the south by the Walton fault zone and the Enriquillo–Plantain Garden fault zone.
microplate rotation - exhumation of continental crust through the process of the subducting plate reversing in motion and rotating due to changing boundary conditions. [ 3 ] crustal stacking - extrusion of weak buoyant material due to the detachment of two layers, a weak buoyant layer atop a stronger negatively buoyant layer, once buoyancy ...
This resulted in the current state of the Macquarie triple junction and is interpreted as a ridge–fault–fault triple junction that now involves a Macquarie microplate rather than the Indo-Australian plate as was the case before 6 million years ago, Pacific plate and Antarctic plate. [2]: 146–149
In the development stages of the microplate, the Pacific plate also shared a coupled shear section to the south of the microplate and, together with the Nazca plate, drove fast rotation of the microplate. [7] [10] Approximately 2.5 Ma ago the Juan Fernández microplate began decoupling from the Pacific plate and coupling with the Antarctic plate.