石油与天然气地质 ›› 2021, Vol. 42 ›› Issue (3): 738-746.doi: 10.11743/ogg20210318
收稿日期:
2021-01-25
出版日期:
2021-06-28
发布日期:
2021-06-23
作者简介:
李平平(1980—),男,副教授,碳酸盐岩储层地质学和油气成藏机理。E-mail: 基金资助:
Pingping Li1,2(), Chun Wang1,2, Huayao Zou1,2, Xinya Yu3
Received:
2021-01-25
Online:
2021-06-28
Published:
2021-06-23
摘要:
碳酸盐的团簇同位素(Δ47)可以直接确定矿物的形成温度,结合矿物的氧同位素,还可以根据传统的氧同位素温度计确定矿物生长的流体(水)的氧同位素(δ18O),提供了一种潜在的确定白云化流体的δ18O、分析白云岩化流体来源的新方法。受白云岩化之后的重结晶作用和高温固态重置作用的影响,白云岩的团簇同位素温度(TΔ47)会比白云化作用实际发生时期的温度偏高,给直接利用TΔ47来恢复白云岩化流体的δ18O造成了一定的局限性。为了分析四川盆地东北部地区长兴组-飞仙关组白云岩化流体的来源,开展了普光气田和元坝气田的白云岩团簇同位素研究。普光气田和元坝气田长兴组-飞仙关组白云岩的TΔ47在70~130 ℃,是重结晶作用和固态重置之后的白云岩视平衡温度。根据地层温度演化史和白云石的固态重置模型,固态重置作用导致川东北地区白云岩的平衡温度增高了30~35 ℃。经固态重置恢复之后确定的白云化流体的δ18O(SMOW)在0~4‰,表明白云岩化流体来源于高盐度的蒸发流体。
中图分类号:
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