Oil & Gas Geology ›› 2020, Vol. 41 ›› Issue (1): 177-188.doi: 10.11743/ogg20200116
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Lingfang Zhou1,2(), Yixiong Qian1, Xiaobo Song3, Bo Cao3, Donghua You1, Yong Li3
Received:
2019-08-08
Online:
2020-02-01
Published:
2020-01-19
Supported by:
CLC Number:
Lingfang Zhou, Yixiong Qian, Xiaobo Song, Bo Cao, Donghua You, Yong Li. Characteristics, distribution and origin of dolomite reservoir in the upper Lei 4 member of the Middle Triassic, Pengzhou gas field, western Sichuan Basin[J]. Oil & Gas Geology, 2020, 41(1): 177-188.
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Table 1
Classification of reservoir space for carbonate rocks in the upper Lei 4 member of the Middle Triassic in Pengzhou gas field"
类型 | 组构选择性 | 种类及特征 |
A | 组构选择性溶蚀 | 粒间孔IP、晶间孔BC、粒内孔WP、窗格孔FE、遮蔽孔SH,铸模孔MO、与生物有关格架(GF)、微生物席(凝块、核形石、藻纹层-叠层石等)藻菌有关的有机孔OM、膏溶模孔、生物扰动-钻孔-遗迹、潜穴BO-BU等 |
B | 组构-非组构溶蚀 | 角砾间(溶)孔,窗格溶孔(洞)、膏溶孔洞、各种残余孔(洞)等 |
C | 裂隙-非组构溶蚀 | 张扭裂隙、压扭剪切(X共轭、雁行排列)、扩溶缝(洞)、溶孔洞(穴)、溶沟-渠道等 |
D | 微孔隙 | 0.02~10 μm孔隙,泥晶白云石、方解石晶间微孔;凝块、叠层石、藻纹层中微孔、粘土有机质中微孔以及晶体内微孔(石膏、天青石、萤石、黄铁矿等) |
Fig.4
A diagram exhibiting the lithology, pore types, physical properties and well-logging responses for the cored interval (6-8 roundtrips) in the Lei 4 member in Well YS1 in Pengzhou gas field (data of porosity, permeability and high pressure mercury injection(HPMI) are the courtesy of Southwest Oil and Gas Branch of SINOPEC)"
Table 2
Characterization parameters for pores of dolomites with various microbial textures and silty-micritic and micritic dolomites sampled from Well YS1 in Pengzhou gas field"
岩石类型 | 储集空间 | 孔隙结构 | 排驱压力/MPa | 孔喉半径/μm | 孔隙度/% | 渗透率/(10-3 μm2) |
泥微晶白云岩 | 微裂隙和微孔隙 | 纳米孔喉,连通性差 | | |||
微粉晶白云岩 | 晶间(溶)孔 | 大孔喉,连通性好 | | | | |
藻凝块(藻团块)白云岩 | (藻)格架孔、粒间(溶)孔 | 亚微米孔喉,连通性一般 | | | | |
藻球粒(藻砂屑)白云岩 | (藻)格架孔、粒间(溶)孔和微孔隙 | 亚微米孔喉,连通性一般 | | | | |
藻纹层藻粘结白云岩 | (藻)格架孔晶间(溶孔) | 大孔喉,连通性好 | | | | |
Table 3
The reservoir assessment in terms of lithology, pore type and physical property for the upper Lei 4 member of the Middle Triassic in Pengzhou gas field"
储层分类 | Ⅰ | Ⅱ | Ⅲ | Ⅳ(致密层) |
孔隙度/% | >10 | 10~5 | 5~2 | < 2 |
渗透率/(10-3 μm2) | >5 | 5~0.1 | 0.1~0.01 | < 0.01 |
平均孔喉半径/μm | >0.3 | 0.3~0.1 | 0.1~0.05 | < 0.05 |
主要岩石类型 | 藻纹层-球粒、叠层石云岩、藻纹层-藻粘结云岩及藻砂屑(凝块)云岩、粉细晶云岩 | 藻球粒-藻纹层-藻粘结云岩、粉(细)晶云岩、藻凝块云岩、藻砂屑(凝块)云岩 | 残余藻球粒(或纹层)(含灰)泥粉晶云岩、砂屑(凝块)-藻粘结云岩、含灰粉晶云岩 | 含灰(膏)泥(粉)晶云岩、含云的泥晶灰岩或藻粘结灰岩、含云的生屑泥晶灰岩 |
孔隙类型 | 窗格(扩)溶孔洞、藻格架孔、溶孔洞、粒内溶孔、晶间(溶)孔及裂隙、扩溶缝、角砾状溶孔 | 晶间(溶)孔、窗格(扩溶)孔、粒内(间)孔、溶孔(洞)、残留孔隙、微裂隙、扩溶缝 | 晶间孔、粒内孔(微孔隙)、窗格孔、角砾状孔、微裂隙、铸模孔、扩溶缝、残余孔 | 晶(粒)间孔、粒间(内)孔、微孔隙 |
其他特征 | 无或较弱的胶结、油斑或油迹 | 白云石、方解石胶结或充填等、少量油斑 | 去云化、白云石、方解石胶结或充填等 | 微生物矿化、白云岩化、去云化、石膏胶结 |
Table 4
The lithology, microfacies, depositional cycle, and diagenesis of the cored interval, and the correlation of pore development and physical property in Well PZ1 in Pengzhou gas field"
埋深/m | 层段 | 主要岩性 | 微相与旋回 | 成岩作用(胶结类型及比例) | 不同类型孔隙比例 | 实测物性 |
5 763.95~ 5 767.77 | T2l4 (3-1) | 有孔虫球粒-砂屑-核形石灰岩 | SMF18, 21, 13 | C0-CⅠ(1%0~15%)、剩余孔隙1%~2%、溶缝孔5%~10%(CⅠ-CⅡ)全部胶结,缝合线白云化(1%~3%),微裂隙孔隙1%~2% | 溶缝31%,BC-IP16%,藻溶孔53%(n=19) | 孔隙度< 2%,个别样品达4%,渗透率< 0.1×10-3 μm2 |
5 808.00~ 5 815.30 | T2l4 (3-2) | 砂屑-球粒-叠层石白云质灰岩 | 向上变深, SMF11, 16, 21, 19 | 泥晶套 | 溶缝17%,MO+FE(7.0%),BC-IP27%,藻溶孔27.6%(n=29) | |
残余藻球粒-粉晶-泥晶白云岩、灰质白云岩 | 雾心亮边、去白云化、偶含硬石膏、扩溶缝 | 孔隙度为2%~5%,渗透率介于0.01×10-3~0.1×10-3μm2 | ||||
5 817.80~ 5 821.00 | T2l4 (3-3) | 粉晶-凝块-球粒-微晶与凝块白云岩夹薄层残余藻球粒灰质白云岩 | 2个向上变深, SMF17,13 | 非组构扩溶缝洞、FE、渗流砂 | 溶缝18.8%,MO+FE(8.3%),BC-IP41.7%,藻溶孔31.25%(n=29) | 孔隙度部分大于5%,渗透率介于0.1×10-3~10×10-3 μm2 |
5 821.60~ 5 825.80 | T2l4 (3-4) | 砂屑-凝块-球粒-泥晶白云岩 | 向上变浅, SMF16 | 棘皮(纤状C00+粒状C01:10%)-巨晶CⅡ(20%~30%),云化50%~60%(5 821.88 m),溶孔(CⅠ)+裂隙CⅠ(10%)(5 822.95 m) | 孔隙度为2%~3%,渗透率介于0.1×10-3~1.0×10-3 μm2 | |
5 825.80~ 5 828.80 | 含生屑球粒-凝块-粉晶-砂屑灰质白云岩 | 向上变深 | 砂屑-凝块(纤状-粒状C00-C01, 10%),溶孔CⅠ(5%~8%),MO(1%~2%); FE5%~8%,CⅠ,扩溶孔,泡沬状,FE3%~5%(CⅠ1%~2%胶结) | |||
粉晶-泥粉晶-粉细晶白云岩 | 强白云化, SMF18 | 晶间孔、晶间溶孔、微裂隙 | 孔隙度为2%~5%,渗透率介于0.1×10-3~1.0×10-3 μm2 |
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