Burial diagenesis of carbonate rocks

碳酸盐岩的埋藏成岩作用

• 批准号: 37228-2008
• 负责人: Machel, Hans
• 金额: $ 2.91万
• 依托单位: University of Alberta
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2009
• 资助国家: 加拿大
• 起止时间: 2009-01-01 至 2010-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=421080
• 关键词: Burial; diagenesis; carbonate; rocks

"Diagenesis" comprises all mineralogical, physical, and chemical changes that happen to sedimentary deposits from the time of deposition at the Earth's surface to burial at depths of about 6 - 9 km and commensurate temperatures of about 200 oC. Diagenesis is of supreme importance for human civilization. Because of the changes in porosity and permeability, diagenesis affects the ability of the rocks to carry or store groundwater (used for human consumption and irrigation in relatively shallow settings), oil and gas (commonly in deeper settings), and certain metal ores (shallow or deep settings).

“成岩作用”包括沉积沉积物从地表沉积到埋藏在约6-9千米深处、相应温度约200摄氏度时发生的所有矿物学、物理和化学变化。成岩作用对人类文明具有极其重要的意义。由于孔隙度和渗透率的变化，成岩作用会影响岩石携带或储存地下水(在相对较浅的环境中用于人类消费和灌溉)、石油和天然气(通常在较深的环境中)以及某些金属矿石(浅或深环境)的能力。