安徽宿松栖霞组古代上升流强度及其特征
he characteristics and Strength of Ancient Upwelling from the Qixia Formation in the Susong Area, Anhui Province
对古代上升流强度的表征方法目前还没有统一认识,古代上升流沉积的厚度可通过野外观察获取,采用上升流累积沉积厚度占层厚的百分比来计算上升流强度,进而分析上升流强度的演化特征。研究区栖霞组上升流沉积主要集中在7-14层和17-21层,从下到上,上升流强度总体呈现出弱→强→弱的变化趋势。在相同微相内上升流强度从下到上呈现出由强→弱的变化特征。在发育的四种上升流微相中,硅质岩微相上升流强度最大,含燧石条带泥晶灰岩微相上升流强度最低,上升流强度过高或过低,都会对优质烃源岩的形成不利,研究认为上升流强度在20%-50%之间时可形成优质烃源岩。
No consensus has been reached yet about the characterization method of Ancient Upwelling,the thickness of deposition can be obtain by the field observation, adoption of percentage of upwellingmale accumulation deposit thickness to layer thickness are calculated the upwelling strength,the evolution feature of upwelling strength is then analyzed. The upwelling deposit of Qixia Formation is mainly in 7-14 layers and 17-21 layers,from bottom to top ,the upwelling strength shows the change tendency from weakness to strength to weakness. Under the same sedimentary microfacies,the upwelling strength shows the change characteristic from strength to weakness. In the four sedimentary microfacies of upwelling, the greatest upwelling strength is silicalite microfacies, the lowest upwelling strength is chert strip micritic microfacies,too high or too low strength of the upwelling is bad to form the fine hydrocarbon source rocks, the research suggested that the fine hydrocarbon source rocks can form while the upwelling strength in the range of 20%-50%.
胡望水、柴华
石油天然气地质、石油天然气勘探地质学
上升流强度栖霞组古代上升流安徽宿松
Upwelling StrengthQixia FormationAncient UpwellingSusong Area of Anhui Province
胡望水,柴华.安徽宿松栖霞组古代上升流强度及其特征[EB/OL].(2012-05-10)[2025-08-18].http://www.paper.edu.cn/releasepaper/content/201205-169.点此复制
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