石油与天然气地质 ›› 2020, Vol. 41 ›› Issue (4): 696-709.doi: 10.11743/ogg20200404
收稿日期:
2020-03-16
出版日期:
2020-08-01
发布日期:
2020-08-11
第一作者简介:
薛永安(1963-),男,博士、教授级高级工程师,矿产普查与勘探。E-mail:基金项目:
Yong'an Xue(), Feilong Wang, Guomin Tang, Xinqi Li
Received:
2020-03-16
Online:
2020-08-01
Published:
2020-08-11
摘要:
渤海海域是渤海湾盆地新生代的沉降中心,在古近系发育了东营组三段、沙河街组一段-二段(沙一二段)和沙河街组三段3套主力烃源岩,具有丰富常规和非常规石油资源,页岩油气作为重要的非常规资源在渤海海域具有巨大的勘探潜力。基于渤海海域勘探开发实际情况,通过与国内外典型页岩油气盆地石油地质条件对比,综合烃源岩地球化学参数、测井资料、镜下薄片观察及X射线衍射全岩矿物分析等,并结合盆地模拟手段,明确了渤海海域页岩油气的资源潜力,并指明了勘探方向及有利目标。研究结果表明:1)渤海海域4个富烃凹陷主力烃源岩品质好,都有利于形成页岩油气,其中渤中凹陷烃源岩成熟度高,形成页岩气可能性更大,黄河口凹陷和辽中凹陷成熟度相对较低,更易形成页岩油,歧口凹陷东三段和沙一二段成熟度低,易形成页岩油,其沙三段成熟高,易形成页岩气;2)3套主力烃源岩脆性矿物平均含量超过63.5%,粘土矿物平均含量低于34.7%,具有良好的可改造性,在3 200 m以深泥页岩进入中成岩B期,伊蒙混层中的蒙脱石大量向伊利石转换,增加了页岩储层的可改造性,结合国内外勘探实践认为3 200~4 200 m是渤海海域页岩油气勘探开发的有利深度范围;3)渤中凹陷是渤海海域页岩油气资源潜力最大的凹陷,总资源量高达95.8×108 t,占据渤海页岩油气资源的45.2%,主力烃源岩整体处于超压状态,结合渤海勘探开发的经济成本,渤中凹陷东三段和沙一二段烃源岩埋深适中、成熟度高,是目前渤海海域页岩气勘探最有利层位;4)渤中凹陷西斜坡处于凹陷边缘,3套烃源岩整体处于异常高压且埋深适中,平均TOC值超过3.04%,页岩层段气测全量达到99%,X衍射矿物显示该区页岩储层中粘土矿物含量较渤海其他区域最低,具备更好的可压性,可作为渤海现阶段最有利目标区。
中图分类号:
表1
国内外页岩油气及渤海海域富烃凹陷泥页岩特征"
类型 | 地区 | 泥页岩名称 | 环境 | 层系 | 埋深/km | 厚度/m | TOC/% | Ro/% | 有机质类型 |
页岩油 | 北美[ | Bakken | 海相烃源岩 | C1 | 1.8~2.7 | 5~15 | 7.23~12.90 | 0.65~0.90 | Ⅱ型 |
Niobrara | K2 | 2.4~2.7 | 80~140 | 2~8 | 0.6~1.3 | Ⅱ型为主 | |||
Barnett | C1 | 1.98~2.60 | 67~90 | 4~8 | 0.6~1.4 | Ⅱ型 | |||
Eagle Ford | K2 | 1.2~4.5 | 30~90 | 1~7 | 1.15~1.40 | Ⅰ型、Ⅱ型 | |||
Monterey | N1 | 2.130~4.267 | 914~1220 | 0.7~5.6 | 0.3~1.1 | Ⅱ型 | |||
沧东凹陷[ | 孔二段 | 陆相烃源岩 | E | 1.8~3.8 | 50~350 | 0.34~8.51 | 0.54~0.82 | Ⅰ型、Ⅱ1型 | |
吉木萨尔凹陷[ | 芦草沟组 | P | 3.0~4.5 | 100~320 | 0.75~3.83 | 0.66~1.63 | Ⅱ型为主 | ||
鄂尔多斯盆地[ | 延长组长7段 | T | 1.5~3.5 | 100~140 | 6~22 | 0.85~1.15 | Ⅰ型、Ⅱ1型 | ||
页岩气 | 北美[ | Ohio | 海相烃源岩 | D | 0.610~1.524 | 91~610 | 0.5~23.0 | 0.4~4.0 | Ⅱ型 |
Antrim | D | 0.183~0.730 | 49 | 0.3~24.0 | 0.4~0.6 | Ⅰ型 | |||
NewAlbany | D | 0.183~1.494 | 31~122 | 1~25 | 0.4~0.8 | Ⅱ型 | |||
Barnett | C | 1.981~2.591 | 61~300 | 1~13 | 1.0~2.1 | Ⅱ型 | |||
Lewis | K | 0.914~1.829 | 152~579 | 0.45~3.00 | 1.60~1.88 | Ⅲ型为主,少量Ⅱ型 | |||
四川盆地[ | 龙马溪组 | S1 | 1.6~3.6 | 80~180 | 1.88~4.36 | 2.6~3.6 | Ⅰ型、Ⅱ1型 | ||
筇竹寺组 | 2.5~4.2 | 100~400 | 1.5~5.7 | 3.0~4.2 | |||||
渤中凹陷 | 东三段 沙一二段 沙三段 | 陆相烃源岩 | E | 2.5~6.0/3.8 | 80~500/150 | 0.35~4.07/1.26 | 0.52~2.20/1.23 | Ⅱ型为主,少量Ⅲ型 Ⅱ型为主,少量Ⅰ型 Ⅱ型为主 | |
2.7~6.5/4.4 | 50~300/130 | 0.25~6.90/1.87 | 0.53~2.80/1.43 | ||||||
2.7~7.3/5.0 | 100~1000/215 | 0.34~7.76/1.78 | 0.54~3.60/1.77 | ||||||
辽中凹陷 | 1.1~4.1/2.5 | 70~295/150 | 0.2~2.5/1.5 | 0.31~1.80/0.84 | |||||
1.3~6.0/3.4 | 20~140/70 | 0.25~4.50/1.60 | 0.31~2.30/0.93 | ||||||
1.5~6.8/3.6 | 90~350/220 | 0.46~2.50/1.63 | 0.31~3.40/1.19 | ||||||
黄河口凹陷 | 2.0~4.1/3.2 | 80~370/135 | 0.1~2.8/1.1 | 0.51~1.20/0.79 | |||||
2.2~4.5/3.5 | 10~150/50 | 0.11~4.55/1.25 | 0.51~1.40/0.85 | ||||||
2.2~4.5/3.6 | 90~1000/230 | 0.22~9.19/1.60 | 0.51~2.10/1.03 | ||||||
歧口凹陷 | 1.8~4.3/3.2 | 60~300/130 | 0.10~3.15/1.10 | 0.45~1.20/0.79 | |||||
1.80~5.00/3.65 | 50~290/150 | 0.10~2.76/1.80 | 0.45~1.80/0.94 | ||||||
1.9~6.6/4.1 | 100~600/200 | 0.05~3.76/1.73 | 0.47~4.00/1.66 |
表2
渤海海域及国内外海相、陆相页岩矿物含量"
地区 | 层位 | 盆地/凹陷 | 矿物含量/% | |||||
石英 | 长石 | 方解石 | 白云石 | 黄铁矿 | 粘土矿物 | |||
北美 | Barnett | Fort Worth盆地[ | 3.0~69.0/28.8 | 0~5.0/1.8 | 0~91.00/36.74 | 0~5.0/1.4 | 0~29.0/1.5 | 7~48.0/24.2 |
Eagle Ford | Gulf of Mexico盆地[ | 均值13.9 | 0~12.0/3.4 | 4~90/58 | 0~48.0/3.5 | 均值2.4 | 0~73.0/30.4 | |
Bakken | Williston盆地[ | 22.0~90.0/64.2 | 3~16.0/9.1 | 0~5.0/1.2 | 1~9.0/3.4 | 均值4.4 | 1.0~46.0/21.5 | |
四川 | 龙马溪组 | 四川盆地[ | 12.0~73.0/36.1 | 6.5~12.7/8.8 | 5.6~12.1/9.2 | 4.0~10.4/7.6 | 1~1.9/1.4 | 16.0~70.0/41.6 |
大港 | 孔二段 | 沧东凹陷[ | 10.0~25.0/15.7 | 5.0~30.0/17.3 | <20.0/8.2 | 0~50.0/27.2 | <3.0 | 5.0~25.0/13.0 |
渤海 海域 | 东三段 | 渤中凹陷 | 16.0~40.0/25.9 | 2.0~23.0/7.0 | 2.0~26.0/17.2 | 1.0~13.0/4.7 | 0~5.0/2.2 | 30.0~52.0/38.0 |
辽中凹陷 | 29.0~57.0/42.3 | 11.0~34.0/19.7 | 2.0~14.0/5.1 | 0~5.0/1.9 | 0~1.0/0.1 | 19.0~47.0/33.6 | ||
黄河口凹陷 | 20.0~61.0/38.6 | 13.0~27.0/20.7 | 1.0~8.0/3.8 | 0~2.0/1.2 | 0~1.0/0.1 | 11.0~44.0/32.4 | ||
歧口凹陷 | 18 | 9 | 31 | 6 | 2 | 30 | ||
沙一二段 | 渤中凹陷 | 16.0~34.0/24.5 | 2.0~15.0/5.9 | 7.0~42.0/18.9 | 3.0~22.0/10.2 | 1.0~6.0/3.2 | 21.0~46.0/33.9 | |
辽中凹陷 | 32.0~48.0/37.7 | 23.0~29.0/26.7 | 2.0~4.0/3.3 | 0~2.0/1.3 | 少见 | 24.0~32.0/28.7 | ||
黄河口凹陷 | 11.0~43.0/32.8 | 10.0~43.0/23.6 | 0~24.0/2.0 | 0~66.0/5.5 | 0~5.0/0.4 | 6.0~54.0/31.7 | ||
歧口凹陷 | 20 | 9 | 25 | 4 | 5 | 33 | ||
沙三段 | 渤中凹陷 | 17.0~30.0/23.3 | 3.0~21.0/10.3 | 2.0~33.0/13.5 | 3.0~20.0/9.8 | 1.0~5.0/2.5 | 25.0~47.0/37.3 | |
辽中凹陷 | 19.0~46.0/26.7 | 17.0~42.0/29.4 | 1.0~16.0/7.7 | 3.0~5.0/3.8 | 0.0~3.0/1.4 | 7.0~42.0/26.2 | ||
黄河口凹陷 | 19.0~46.0/26.8 | 17.0~42.0/29.5 | 1.0~16.0/7.8 | 0~18.0/6.0 | 0~3.0/1.5 | 7.0~42.0/26.3 |
表3
渤海海域典型地区陆相页岩矿物含量"
凹陷 | 矿物含量/% | ||||||
石英 | 长石 | 方解石 | 白云石 | 黄铁矿 | 粘土矿物 | ||
渤中凹陷 | CFD23-2-1井区 | 15.0~35.0/23.4 | 10.0~36.0/22.6 | 3.0~25.0/8.8 | 0~17.0/9.4 | 0~3.0/0.5 | 5~43/26 |
渤中13-1 | 7.5~57.0/37.4 | 0.3~42.0/8.3 | 1.7~55.6/15.7 | 0~21.0/3.6 | 0~5.0/1.6 | 16~70/42 | |
渤中19-6 | 16.0~40.0/25.0 | 2.0~23.0/7.6 | 2.0~42.0/16.5 | 1~22.0/6.8 | 0~6.0/2.4 | 21~52/37 | |
歧口凹陷 | 18.0~20.0/19.0 | 9 | 25.0~31.0/28.0 | 4.0~6.0/5.0 | 2.0~5.0/3.5 | 30~33/32 | |
辽中凹陷 | 27.0~57.0/40.8 | 11.0~34.0/20.2 | 2.0~14.0/5.0 | 0~4.0/0.3 | 0~1.00/0.04 | 19~47/34 | |
黄河口凹陷 | 11.0~61.0/33.2 | 10.0~43.0/23.6 | 0~32.0/3.0 | 0~66.0/4.9 | 0~5.0/0.5 | 6~54/32 |
表4
渤海海域页岩粘土矿物特征"
层位 | 井号 | 深度/m | 粘土矿物相对含量/% | 伊/蒙混层比/% | |||
伊利石 | 高岭石 | 绿泥石 | 伊/蒙混层 | ||||
东三段 | BZ19-6-3 | 3 620 | 66 | 5 | 9 | 20 | 20 |
BZ19-6-7 | 4 050 | 64 | 5 | 5 | 26 | 25 | |
BZ19-6-7 | 4 260 | 96 | 1 | 3 | 0 | 0 | |
JX1-2-1 | 2 115 | 45 | 11 | 5 | 39 | 20 | |
沙一二段 | BZ19-6-4 | 4 350 | 98 | 1 | 1 | 0 | 0 |
BZ19-6-6 | 4 005 | 87 | 2 | 2 | 9 | 10 | |
BZ19-6-10 | 4 350 | 71 | 1 | 1 | 27 | 10 | |
BZ27-2-2 | 3 820 | 76 | 4 | 2 | 18 | 10 | |
KL10-2-2D | 2 455 | 20 | 8 | 5 | 67 | 50 | |
沙三段 | BZ19-6-3 | 3 800 | 95 | 3 | 2 | 0 | 0 |
BZ19-6-3 | 3 819 | 80 | 1 | 1 | 18 | 20 | |
BZ19-6-11 | 4 435 | 96 | 1 | 3 | 0 | 0 | |
BZ19-6-11 | 4 445 | 87 | 1 | 3 | 9 | 20 | |
KL10-2-2D | 3 060 | 36 | 7 | 4 | 53 | 15 | |
KL10-2-2D | 3 160 | 39 | 5 | 3 | 53 | 15 | |
LD29-1-2 | 2 825 | 10 | 28 | 18 | 44 | 45 | |
LD29-1-2 | 2 845 | 54 | 3 | 2 | 41 | 20 |
表5
渤海海域富烃凹陷主力烃源岩生烃量"
凹陷 | 东三段 | 沙一二段 | 沙三段 | 总计 |
渤中凹陷 | ||||
辽中凹陷 | ||||
黄河口凹陷 | ||||
歧口凹陷 | ||||
总计 |
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