1) deep burial hot water dolomitization
深埋藏热水云化
2) deep buried hydrothermal dolostones
深埋热液白云岩
1.
The types and genetic mechanism of the Cambrian-Lower Ordovician deep buried hydrothermal dolostones in Yaha-Yingmaili region, Tarim basin are investigated by means of stained thin section microscopic identification, cathodoluminescence microscopic observation, carbon and oxygen isotope geochemistry, trace element analysis, and fluid inclusion analysis.
根据铸体薄片鉴定、阴极发光显微镜观察、碳、氧稳定同位素测定、微量元素分析及包裹体测温等手段,对塔里木盆地牙哈—英买力地区寒武—下奥陶统深埋热液白云岩类型及成因机理进行了详细的研究。
3) burial evolution
埋藏热演化
1.
The differential burial evolution led to the differential thermal evolution in different structural belts.
研究表明:塔里木盆地自下古生界沉积以来,地温梯度整体递减的热史和多次地层抬升剥蚀降温,延缓了烃源岩热演化进程;差异埋藏热演化,使部分地区烃源岩的生烃潜力得以保持至喜山期;晚期的快速深埋升温使短期内大量生、排烃并高效运聚;为新构造期的断裂系统活化提供运移的通道;这些地质条件是下古生界油气可晚期成烃成藏的保证。
4) burial dissollution
埋藏去白云岩化
1.
The burial dissollution porosities deriv.
鄂尔多斯盆地东部下奥陶统碳酸盐岩埋藏成岩事件主要有埋藏白云岩化、埋藏溶解作用、埋藏胶结作用、埋藏去白云岩化、有机质成岩作用和粘土矿物转化作用等。
5) burial dolomitization
埋藏白云石化
1.
The origin of dolomited in the study area can be classified into penecontemporaneous dolomitization, seepoge-reflux dolomitization, dorag dolomitization, pressure solution dolomitization and burial dolomitization.
研究区白云岩成因类型可划分出准同生白云石化、回流渗透白云石化、混合水白云石化、压溶白云石化和埋藏白云石化。
补充资料：雾暗云深
1.迷蒙渺远。喻相距之遥远。
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