1) biogenic gas pool
生物气成藏
1.
Sedimentary facies and biogenic gas pool of the Quaternary of Sanhu area in Qaidam Basin;
柴达木盆地三湖地区第四系沉积相与生物气成藏
2) late biogas accumulation
生物气晚期成藏
3) gas reservoir of biologic origin
生物成因气藏
4) abiogenic gas reservoir
非生物成因气藏
5) biogenetic gas reservoir
生物气藏
1.
The mudstone caprocks of biogenetic gas reservoir of Quaternary in Qaidam Basin is in the early stage of diagenesis, with the characteristics of poor consolidation, relatively high porosity, big pore diameter and relatively lower breakthrough pressure, which results in the weak sealing of biogenetic gas reservoirs.
柴达木盆地第四系生物气藏泥岩盖层处于成岩阶段早期,具有成岩性差、高孔隙度、大孔径、低突破压力的特点,造成生物气藏整体处于弱封闭状态,而大规模气田区的存在,必定有其独特的封闭机理。
6) biogas pool
生物气藏
1.
Under the control of geotectonic evolution zonality and paleogeographic and paleoclimatic zonality of the Cenozoic, five kinds of basic forming models of biogas pools were developed in the Cenozoic basins of China.
受新生代大地构造演化分区及古地理、古气候分区的控制,我国新生代盆地发育 5 种生物气藏的基本形成模式。
补充资料：煤层气(见煤成气)
煤层气(见煤成气)
coal-bed gas:see coal derived gas
于煤煤层气(c oal一bed gas)以吸附状态赋存 层内部的煤成气。见谋成气。-
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条