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The X-ray fluorescence(XRF)core-scanned Rb/Sr ratios of lake sediments have been widely used as a proxy for chemical weathering intensity and past climate change.However,some factors could affect Rb/Sr ratios,causing misinterpretation and limiting its application.In this study,we present a high-resolution XRF core-scanned Rb/Sr record of core ZB13-C1 from the Zoige Basin in the eastern Tibetan Plateau.To validate its application,we correlated this record with the chemical index of alteration(CIA)and other paleoclimatic proxies.Our results showed that(1)the core-scanned Rb/Sr ratios and CIA were reliable proxies of chemical weathering intensity in fine-grained sedimentary sequences;(2)the low values of corescanned Rb/Sr ratios and CIA were significantly correlated with high total organic carbon content,arboreal pollen content,carbonate content,and C/N ratios,confirming its reliability as a proxy for the Asian summer monsoon intensity;(3)the corescanned Rb/Sr ratios at core depths of 25–0.3 and 56–47 m were unable to reliably reflect chemical weathering intensity due to both the grain-size effect and the low test accuracy.Our study highlights the need for mutual verification of multiple indicators before accurately applying Rb/Sr as a paleoclimatic proxy in other similar study areas.  相似文献   
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郭天婵  唐华风  王寒飞 《地质学报》2021,95(12):3885-3898
侵入岩油气藏广泛分布于世界各盆地中,具有良好的油气勘探潜力.但对原生孔隙发育的岩脉储层模式的研究尚未引起足够的关注.本文以新西兰基督城Lyttelton火山西北部的中新世浅成岩脉为研究对象,根据野外露头调查、孔渗测试、图像分析和经验公式的渗透率计算,对其孔隙构成、储层分布模式和储层控制因素进行分析.结果 表明:该区浅成侵入岩为孔隙-裂缝型储层,储集空间以气孔为主,冷凝收缩缝次之;气孔可见定向拉长的大直径椭圆形和离散的小直径圆形两类,对孔隙度的贡献以前者为主;柱状节理可见规则和不规则两类,后者的裂缝面密度较高;具有中孔-中渗的特征,局部高孔-高渗;柱体横截面形态和规则性是影响地层渗透性的关键因素.整体上,浅成岩脉从下到上孔隙度由小变大,柱状节理由规则变为不规则;气孔可由柱状节理沟通,其连通性受柱状节理缝间距、缝宽,以及定向拉长气孔与柱状节理之间的夹角控制;Lyttelton火山的浅成岩脉显示,冷凝固结阶段气孔的初始连通率可高达35%.综上,浅成岩脉可具有良好的储集性能,气孔初始连通性较高,可作为有利的勘探目标.  相似文献   
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新西兰Taranaki盆地中新世Kora火山是海底喷发形成的碎屑岩型火山,可代表浅埋藏火山岩的储层特征.本文根据5口钻井的孔隙度、渗透率、孔隙孔径和铸体薄片开展Kora火山的储层特征、储集空间组成、缝宽以及原生和次生孔隙之间关系的分析.研究结果如下:(1)储集空间主要为次生孔隙,然后是裂缝和原生孔隙;Kora火山具有高...  相似文献   
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