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Based on the studies by Itoh et al. (2005) and information from Oryzabase (http://www.shigen.nig.ac.jp/rice/oryzabase/top/top.jsp), rice panicle and seed developmental stages were divided into 6 and 5 major categories, respectively.
In this study, the diagenetic evolution sequence was determined by thin-section identification; then, inclusion formation stages were divided according to the host minerals' formation sequence combined with the inclusion petrography analysis.
The hydrocarbon charge stages were divided qualitatively based on the analysis of generation and expulsion stages of major hydrocarbon source rocks and fluorescence microscopic features (Jarmołowicz-Szulc et al. 2012); the hydrocarbon fluid inclusion forming periods were divided according to the diagenetic evolution sequence of host minerals combined with reservoir burial evolution history.
The Giro's 21 stages were divided into the following classifications by race organizers Gazzetta dello Sport: four time trials (three individual and one team), seven flat stages, five mixed stages, and six mountain stages.
The Giro's twenty-one stages were divided into the following classifications: three time trials (one team and two individual), eleven flat or undulating stages (officially there was no distinction made between flat and undulating), four intermediate stages, and three mountain stages.
Additionally, for analytical studies, pistils from different developmental stages were divided into two parts, stigma with style and ovary, by using a razor blade.
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Production stages are divided for each well by the value of dimensionless gas production rate (Table 2).
If the CBM production stages are divided by gas production rate, then gas production data can be directly used for division of stages.
Thereby, the fluidized bed compartments or stages are divided from each other by weirs with defined openings (slots) for particle exchange.
The four stages are divided: initial degradation stage, for MAGT ≤ − 2.5 °C; the intensive degradation stage, for − 2.5 °C < MAGT ≤ − 0.5 °C; the vertical talik stage, for − 0.5 °C < MAGT ≤ 0 °C; and the quasi-disappearance stage, for MAGT > 0 °C.
There are two main schemes for dividing the CBM well production stages as follows: (1) Four stages are divided based on the characteristics of the change in fluid phase, including saturated single-phase flow of water, unsaturated single-phase flow of water, two-phase flow of gas and water, and single-phase flow of gas stages (Ni et al. 2010).
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