1) homogeneous temperature in inclusion enclaves
包裹体均-温度
2) homogenization temperature of fluid inclusions
包裹体均一温度
1.
With the homogenization temperature of fluid inclusions, the paleo-geotemperature gradient of the strata in different geologic times in the middle part of Sichuan Basin can be calculated on the basis of an integrated analysis of the depositional_burial history of the Basin, the main geothermal events, the data of logging temperature and vitrinite reflectance ( R o) from the cores of wells.
根据四川盆地沉积－埋藏史、主要地热事件、井下Ｒｏ剖面及钻井测温资料的综合分析，应用流体包裹体均一温度资料推算了四川盆地中部各地质时期地层的古地温，并建立了古地温梯度表，用此表可计算四川盆地各时期地层古地温。
3) fluid inclusions homogenization temperature
流体包裹体均一温度
4) inclusion thermometry
包裹体测温
1.
By means of inclusion thermometry and authigenic illite dating data,the oil and gas migration and accumulation model in the central anticlinal zone in the Xihu Sag of the East China Sea Basin has been studied.
利用包裹体测温和成岩矿物伊利石测年数据资料,对东海盆地西湖凹陷中央背斜带油气运移及成藏的基本模式进行了研究。
5) temperature measuring of fluid inclusion
流体包裹体测温
6) fluid inclusion microthermometry
包裹体测温法
1.
Thermal history of TWT-2 well in the central anticline belt in Xihu Depression is reconstructed using the methods of combination and fluid inclusion microthermometry.
利用结合法与流体包裹体测温法能有效地恢复含油气盆地的热演化历史。
补充资料：包裹体
见包裹体地球化学、地质温度计。
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