收稿：2018-04-02，
纸质出版：2020-06-28
移动端阅览
塔里木盆地下古生界碳酸盐岩广泛发育，是油气勘探的重要领域。以塔里木盆地塔河、玉北地区下奥陶统为例，通过岩心观察、薄片鉴定、电子探针、C、O、Sr同位素
以及REE元素分析，结合测井及地震资料，探讨了断裂系统和层序地层格架中的热液活动及成储效应。研究认为：中-细晶白云岩遭受富硅质热液流体改造强烈，表现为热褪色现象、鞍状白云石充填和充填白云石、方解石、玉髓、黄铁矿等多种矿物组合沉淀，以及较高的SiO
2
、FeO、MnO、BaO含量、较低的SrO含量和
87
Sr/
86
Sr值、偏负的δ
18
O值、较低的∑REE含量、明显的Eu正异常和Ce负异常。热液流体对白云岩储层的改造主要表现为溶蚀作用、重结晶作用和充填作用三个方面，溶蚀作用形成的次生溶蚀孔隙成为最重要的储集空间。不同尺度断裂和三级层序甚至更短周期层序界面共同构成深部热液流体运移的输导体系，对热液活动及储层发育起到强烈的控制作用，并建立了塔里木盆地塔河、玉北地区下奥陶统蓬莱坝组断裂-层序双控机制下的热液活动及成储效应的概念模型。
The Lower Paleozoic carbonate rocks in the Tarim Basin are widely developed
representing an important target of hydrocarbon exploration.Taking the Lower Ordovician in Tahe and Yubei areas in the Tarim Basin as examples
we discussed the impact of hydrothermal activities on reservoir formation in the fault belts and along stratigraphic framework
through core and thin section observation
electron probe microanalysis (EPMA)
seismic and logging data
as well as the analyses of C
O
and Sr isotopes and REEs.The results show that medium to fine-crystalline dolomites are strongly modified by silica-rich hydrothermal fluids.A series of characteristics occurred as a result of this process
such as:thermal fading
saddle dolomite filling
and mineral precipitation including dolomite
calcite
chalcedony
pyrite and so on
as well as higher SiO
2
FeO
MnO and BaO contents
lower SrO contents and
87
Sr/
86
Sr values
more negative δ
18
O values
lower ∑REE contents
obvious positive Euanomalies and negative Ce anomalies.While the dolomite reservoir transformation resulted from hydrothermal fluids mainly includes dissolution
recrystallization and filling
the secondary pores with dissolution serve as the most important reservoir space.The conduit system for deep hydrothermal fluid migration is composed of faults of various scales
third-order sequences boundaries
or sequence boundaries of even shorter periods
playing a deci-sive role in controlling hydrothermal activities and reservoir de
velopment.Finally
a conceptual model displaying the impact of hydrothermal activities on reservoir formation was established under the dual control of faults and sequences boundaries in the study area.
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