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In the Overgrowth phase, tumor cells grow outside the basement membrane of the tissue compartment in which they originated due to increasing scarcity of essential resources, such as oxygen and glucose, that are necessary for further growth and cell division.
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To address concerns of long-term viability (>60 days) and cell overgrowth, stationary phase cells were also tested in the microfluidic channel.
The single layers are 0.5 1.5 cm thick and represent overgrowth of mineral phases.
The overgrowth of mineral phases in the sample is also visible in its chemical composition.
– plane-polarized light; FL fluorescence; Q1 Quartz overgrowth in the first phase; Q 2 Quartz overgrowth in the second phase Open image in new window Fig. 9 Fluid inclusion homogenization temperatures of the two phases of quartz overgrowths of the low permeability Es 3 z turbidite reservoirs.
The II and III phase quartz overgrowth and cement development are important factors for sandstone tight.
The carbonate cement and the I phase quartz overgrowth did not develop well, and thus they have small influence on reservoir quality.
This resulted in the precipitation under appropriate conditions of authigenic kaolinite and first phase quartz overgrowths.
These acidic fluids could dissolve feldspars and carbonates, forming third phase quartz overgrowths with fluid inclusions with homogenization temperatures from 140 to 160 °C (Table 2).
The organic acids dissolved carbonate cements and small amounts of feldspars, which caused second phase quartz overgrowths to develop in the reservoirs.
The first phase of quartz overgrowth is dark black and the second phase is brown as also described by Lander et al. (2008) and Tournier et al. (2010).
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