Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (3): 693-704.doi: 10.13278/j.cnki.jjuese.20170176
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Sun Haitao1, Zhong Dakang1, Li Yong2, Mao Yakun1, Yang Xianzhang1,2
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Natural Gas Geoscience, 2014,25(12):1903-1912. 图版图版说明a.残余粒间孔,克深2-1-5井,6714.35 m,单片光,箭头所指的残余粒间孔,颗粒边缘平直、无溶蚀痕迹,孔隙多呈三角形,且粒间缺乏胶结物;b.残余粒间溶孔,克深207井,6797.91 m,激光共聚焦照片,箭头所指的孔隙具有左上至右下的定向性,且孔隙呈压扁状,内部见少量早期胶结物的残余;c.晚期粒间溶孔,克深201井,6509.67 m,激光共聚焦照片,箭头所指的孔隙中见到大量粒间胶结物,且胶结物边缘呈锯齿状或港湾状,具有溶蚀特征,整个孔隙未表现出受构造挤压影响的定向性和挤压变形特征,与图版b具有明显区别;d.晚期粒间溶蚀扩大孔,克深202井,6799.7 m,激光共聚焦照片,箭头所指的孔隙与图版c类似,但是孔径大,受溶蚀后颗粒边缘呈现凹凸状,但孔隙同样不具挤压变形特征和定向性;e.粒内溶孔,克深208井,6605.76 m,箭头所指的是颗粒内溶孔,长石或岩屑内部被溶(左侧,单片光),孔隙不规则,溶蚀强时会形成铸模孔,溶蚀弱时常形成微孔隙,荧光薄片(右侧)下易识别;f.杂基微孔和粒间微孔,克深2-1-5井,6717.10 m,左侧为普通铸体薄片单片光,箭头所指表明颗粒内,粒间杂基均被油气侵染,表明存在微孔隙,右侧为荧光薄片,在荧光薄片内清晰可见粒间微孔隙、杂基内微孔隙和粒内微孔;g.粒内微孔和裂缝,克深207井,6870.5 m,场发射扫描照片,箭头所指的粒内微孔为纳米级,且颗粒表面有网状缝,可作为喉道;h.张性缝,克深207井,6798 m,单片光,箭头所指为张性裂缝,沿裂缝溶蚀,裂缝两侧呈港湾状;i.高角度缝,克深8井,6736.38 m,岩心上的直劈缝;j.粒缘缝,克深8003井,6779.22 m,激光共聚焦照片,颗粒压实后,紧贴颗粒边缘形成粒缘缝,可作为有效的渗流通道。 |
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