石油与天然气地质 ›› 2023, Vol. 44 ›› Issue (4): 1054-1066.doi: 10.11743/ogg20230420
• 方法技术 • 上一篇
张坦(), 姚威, 赵永强, 周雨双, 黄继文, 范昕禹, 罗宇
收稿日期:
2022-12-12
修回日期:
2023-03-27
出版日期:
2023-08-01
发布日期:
2023-08-09
第一作者简介:
张坦(1994—),男,工程师,构造与油气成藏。E-mail:基金项目:
Tan ZHANG(), Wei YAO, Yongqiang ZHAO, Yushuang ZHOU, Jiwen HUANG, Xinyu FAN, Yu LUO
Received:
2022-12-12
Revised:
2023-03-27
Online:
2023-08-01
Published:
2023-08-09
摘要:
古地貌的精确恢复对于寻找优质储层及烃源岩优势相带起着十分重要的作用,而剥蚀厚度计算又是古地貌恢复研究中的核心步骤。基于自然伽马曲线数据,利用频谱分析、连续小波变换和经验模态分解等技术手段,建立了塔里木盆地巴麦地区石炭系卡拉沙依组具有相对时间概念的“浮动”天文年代标尺和高精度的地层层序格架,并进一步精确计算了石炭系卡拉沙依组剥蚀厚度。结果显示:①巴麦地区石炭系卡拉沙依组沉积时受天文轨道周期的控制,保存有完整的米兰科维奇旋回;②经验模态分解方法得出的固有模态分量imf3与长偏心率(e1)控制下的地层旋回个数基本一致,据此建立了研究区具有相对时间概念的“浮动”天文年代标尺和高精度的地层层序格架;③基于经验模态分解方法计算的结果,结合不同地区钻井缺失旋回数量和平均旋回厚度之间的关系,精确计算了研究区内石炭系卡拉沙依组剥蚀厚度;④研究区内石炭系卡拉沙依组剥蚀厚度在0 ~ 390 m,剥蚀强度整体表现为“西强东弱”的特征,中部BT5井附近斜坡区域,易形成良好的储集体,是下一步有利的勘探区域。研究提出的思路和方法为类似地区高频地层层序格架的构建、“浮动”天文年代标尺的建立及地层剥蚀厚度的精细计算等提供了参考。
中图分类号:
表2
巴麦地区石炭系卡拉沙依组识别主频与对应米兰科维奇周期的比值"
井名 | 旋回参数 | 主导频率/(1/m) | 主导周期比值 | 天文旋回周期比值 | 单个旋回厚度/m | 误差率/% |
---|---|---|---|---|---|---|
YB1 | e1 | 0.019 5 | 12.03 | 12.17 | 6.410 | 1.17 |
e2 | 0.062 5 | 3.75 | 3.76 | 2.000 | 0.10 | |
e3 | 0.082 0 | 2.86 | 2.85 | 1.524 | 0.19 | |
o1 | 0.191 4 | 1.23 | 1.24 | 0.653 | 1.48 | |
o2 | 0.234 4 | 1 | 1 | 0.533 | 0.05 | |
YB8 | e1 | 0.019 5 | 11.43 | 12.17 | 6.410 | 6.11 |
e2 | 0.062 1 | 3.59 | 3.76 | 2.013 | 4.47 | |
e3 | 0.074 2 | 3.00 | 2.85 | 1.685 | 5.20 | |
o1 | 0.191 4 | 1.16 | 1.24 | 0.653 | 6.40 | |
o2 | 0.222 7 | 1 | 1 | 0.561 | 0.05 | |
HT1 | e1 | 0.021 5 | 12.17 | 12.17 | 5.814 | 0 |
e2 | 0.068 3 | 3.83 | 3.76 | 1.830 | 1.86 | |
e3 | 0.093 8 | 2.79 | 2.85 | 1.333 | 2.26 | |
o1 | 0.209 0 | 1.25 | 1.24 | 0.598 | 0.68 | |
o2 | 0.261 7 | 1 | 1 | 0.478 | 0.00 | |
H3 | e1 | 0.021 5 | 12.27 | 12.17 | 5.814 | 0.79 |
e2 | 0.068 4 | 3.86 | 3.76 | 1.827 | 2.65 | |
e3 | 0.091 8 | 2.87 | 2.85 | 1.362 | 0.63 | |
o1 | 0.207 0 | 1.27 | 1.24 | 0.604 | 2.44 | |
o2 | 0.263 7 | 1 | 1 | 0.474 | 0 |
表4
巴麦地区石炭系卡拉沙依组天文周期和剥蚀厚度"
井名 | 厚度/m | 长偏心率(e1)旋回数/个 | 平均旋回厚度/m | 缺失旋回数/个 | 剥蚀厚度/m |
---|---|---|---|---|---|
YB1 | 284.00 | 44.00 | 6.45 | 24.00 | 154.80 |
YB4 | 306.10 | 60.00 | 5.10 | 8.00 | 40.81 |
YB8 | 212.00 | 35.00 | 6.05 | 33.00 | 199.65 |
YB9 | 255.88 | 38.00 | 6.73 | 30.00 | 202.01 |
YB10 | 267.88 | 42.00 | 6.38 | 26.00 | 165.83 |
LN1 | 305.00 | 60.00 | 5.08 | 8.00 | 40.67 |
PSB2 | 262.00 | 44.00 | 5.95 | 24.00 | 142.91 |
BT4 | 55.00 | 9.00 | 6.11 | 59.00 | 360.56 |
BT5 | 204.00 | 33.00 | 6.18 | 35.00 | 216.36 |
BT6 | 66.00 | 11.00 | 6.00 | 57.00 | 342.00 |
BK8 | 24.00 | 4.00 | 6.00 | 64.00 | 384.00 |
Q5 | 284.00 | 42.00 | 6.76 | 26.00 | 175.81 |
J2 | 90.00 | 15.00 | 6.00 | 53.00 | 318.00 |
H2 | 379.00 | 64.00 | 5.92 | 4.00 | 23.69 |
H3 | 397.00 | 67.00 | 5.93 | 1.00 | 5.93 |
H4 | 216.00 | 35.00 | 6.17 | 33.00 | 203.66 |
HT1 | 393.00 | 66.00 | 5.95 | 2.00 | 11.91 |
BD4 | 351.00 | 58.00 | 6.05 | 10.00 | 60.52 |
K1 | 43.00 | 7.00 | 6.14 | 61.00 | 374.71 |
K2 | 117.00 | 20.00 | 5.85 | 48.00 | 280.80 |
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