准噶尔盆地乌尔禾油田高自然伽马砂砾岩特征及其沉积微相研究&mdash;&mdash;以乌36井区百口泉组为例

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名

邮箱

手机号码

标题

留言内容

验证码

准噶尔盆地乌尔禾油田高自然伽马砂砾岩特征及其沉积微相研究——以乌36井区百口泉组为例

详细信息

中图分类号: TE121.3⁺2

计量

文章访问数: 1262
HTML全文浏览量: 3
PDF下载量: 1006
被引次数: 0

High GR Glutinite Feature and Micro-Sedimentary Facies in Wuerhe Oil-field, Junggar Basin——Taking the Baikouquan Group in Wu 36 Area as an example

摘要

摘要: 基于岩芯编录、测录井资料和薄片分析数据，对准噶尔盆地乌36井区三叠系百口泉组开展了沉积学研究。研究表明，乌36井区百口泉组发育冲积扇沉积体系，扇体内部砂砾岩具有自然伽马异常高的特点，而泥岩具有自然伽马异常低的特点，其原因主要是由于原岩碎屑中富含凝灰岩等高放射性物质，同时沉积物的粒度变化、搬运距离和相带展布控制了砂砾岩自然伽马异常的空间变化，并依据伽马异常的空间变化特点建立了相应的泥质含量计算公式，提出了高自然伽马砂砾岩沉积微相划分的一种新方法。区内主要发育冲积扇扇中辫流线微相、扇中辫流砂岛微相、扇中漫洪带微相和扇缘漫流带微相。精细刻画了各期扇体沉积微相的展布与垂向演化特征，百口泉组三段发育四期扇体，垂向上表现为一个快速水退背景和缓慢水进背景下的沉积演化序列；百口泉组二段发育三期扇体，垂向上表现为退积型演化序列；百口泉组一段则表现为冲积扇扇缘沉积。通过与实际生产对比，本次研究较好地解释了区内生产井的生产状况，验证了利用高自然伽马砂砾岩自然伽马特征研究沉积微相的可行性与实用性。
- 自然伽马异常砂砾岩 /
- 沉积微相 /
- 乌尔禾油田 /
- 准噶尔盆地
Abstract: Based on rock core documentation, well logging analysis and the rock fragment data, we carried out the sedimentology research on the Triassic Baikouquan Group in Wu 36 area of Junggar Basin. This study revealed that the Baikouquan Group developped in alluvial fan system. The glutenite is characterized by unusually high natural gamma and the mudstone is characterized by low inside the alluvial fan. This feature is mainly controlled by the high radioactive substance in the original rock, for example the tuff. The spatial variation in high natural gamma anomaly was influenced by sediment grain size, transport distance and facies distribution. According to the spatial variation characteristics of Gamma anomaly, we established a clay content formula and put forward a new method on the division of sedimentary facies. Our study area mainly develops mid-fan braided stream line microfacies, mid-fan braided stream sand island microfacies, mid-fan sheetflood microfacies and cross flow microfacies in marginal subfacies. We also carefully portrayed the distribution and vertical evolution of these sedimentary microfacies of different stages. The results show that the 3^rdmember in Baikouquan Group developed four fan bodies. There is a sedimentary evolutionary sequence in the vertical profile controlled by fast dereliction and slow retrograding. The 2^nd member in Baikouquan Group developed three fan bodies and presented a retrograding evolutionary sequence in the vertical. The 1^st member in Baikouquan Group performed the alluvial fan marginal sedimentary. Compared with the actual production, this study better explained the production status of the regional producing well and verified the feasibility and practicality of using natural gamma characteristics of high natural gamma glutinite to make research on sedimentary microfacies.
- natural gamma anomaly glutinite /
- micro-sedimentary facies /
- Wuerhe Oilfield /
- Junggar Basin

HTML全文

参考文献(0)

[1]	单祥. 准噶尔盆地阜康凹陷深层二叠系上乌尔禾组致密砂砾岩储层特征、成因及勘探方向 . 沉积学报, 2023, (): -. doi: 10.14027/j.issn.1000-0550.2023.097
[2]	单祥, 郭华军, 陈希光, 郭旭光, 佘敏, 李亚哲. 准噶尔盆地玛西斜坡区百口泉组砂砾岩埋藏溶蚀作用实验模拟研究 . 沉积学报, 2022, 40(5): 1406-1418. doi: 10.14027/j.issn.1000-0550.2021.050
[3]	丁超, 庞燕青, 孟亚玲, 黄钰珑, 李闻东, 张顺存, 郭晖, 李佳思, 张明峰. 准噶尔盆地中拐地区上乌尔禾组富火山碎屑砂砾岩储层的古环境及储层机理研究 . 沉积学报, 2020, 38(4): 851-867. doi: 10.14027/j.issn.1000-0550.2020.054
[4]	厚刚福, 孙靖, 王力宝, 李亚哲, 李啸, 沈金龙, 窦洋, 陈扬, 韩守华. 不同古地貌单元水下分流河道沉积特征及其意义——以准噶尔盆地夏盐地区三工河组二段为例 . 沉积学报, 2019, 37(4): 825-833. doi: 10.14027/j.issn.1000-0550.2018.175
[5]	张丽霞, 柳益群, 向辉, 李红, 周鼎武, 焦鑫, 李哲萱, 南云. 凝灰岩型含油层系特征与成因分析——以准噶尔盆地火烧山油田二叠系平地泉组为例 . 沉积学报, 2018, 36(4): 768-776. doi: 10.14027/j.issn.1000-0550.2018.056
[6]	黄远光, 张昌民, 丁雲, 瞿建华, 朱锐, 潘进, 唐勇, 张磊, 陶金雨. 准噶尔盆地玛湖凹陷百口泉组典型微相砾石定向性定量研究 . 沉积学报, 2018, 36(3): 596-607. doi: 10.14027/j.issn.1000-0550.2018.046
[7]	孙靖, 薛晶晶, 吴海生, 吴爱成, 宋明星, 贾开富. 远源、细粒型浅水三角洲沉积特征与演化——以准噶尔盆地腹部莫索湾地区八道湾组为例 . 沉积学报, 2016, 34(1): 129-136. doi: 10.14027/j.cnki.cjxb.2016.01.012
[8]	单祥, 陈能贵, 郭华军, 唐勇, 孟祥超, 邹志文, 徐洋. 基于岩石物理相的砂砾岩储层分类评价——以准噶尔盆地玛131井区块百二段为例 . 沉积学报, 2016, 34(1): 149-157. doi: 10.14027/j.cnki.cjxb.2016.01.014
[9]	邹妞妞, 史基安, 张大权, 马崇尧, 张顺存, 鲁新川. 准噶尔盆地西北缘玛北地区百口泉组扇三角洲沉积模式 . 沉积学报, 2015, 33(3): 607-615. doi: 10.14027/j.cnki.cjxb.2015.03.019
[10]	. 琼东南盆地深水区中央峡谷沉积微相特征 . 沉积学报, 2013, 31(6): 1114-1121.
[11]	雷卞军. 靖边气田马五1-4亚段沉积微相和成岩作用研究 . 沉积学报, 2010, 28(6): 1153-1164.
[12]	马强. 鄂尔多斯盆地伊陕斜坡中部长6油层组沉积微相及其含油性研究 . 沉积学报, 2009, 27(3): 443-451.
[13]	李双文, 刘洛夫, 张有平, 姚卫江, 靳军, 赵建章, 孙东. 准噶尔盆地莫北凸起侏罗系三工河组沉积演化及微相构成 . 沉积学报, 2006, (6): 819-828.
[14]	李双文刘洛夫张有平姚卫江靳军赵建章孙东. 准噶尔盆地莫北凸起侏罗系三工河组沉积演化及微相构成 . 沉积学报, 2006, 24(06): 819-828.
[15]	鲍志东, 刘凌, 张冬玲, 李儒峰, 管守锐, 康永尚, 王英名, 齐雪峰, 赵秀岐. 准噶尔盆地侏罗系沉积体系纲要 . 沉积学报, 2005, 23(2): 194-202.
[16]	吴胜和, 武军昌, 李恕军, 吴志宇. 安塞油田坪桥水平井区沉积微相三维建模研究 . 沉积学报, 2003, 21(2): 266-271.
[17]	张中宁, 陈国俊, 薛莲花, 王琪. 准噶尔盆地北三台地区湖相原油咔唑类化合物的地球化学特征 . 沉积学报, 2002, 20(1): 160-164.
[18]	杨建业, 任德贻, 邵龙义. 沉积有机相在陆相层序地层格架中的分布特征——以吐哈盆地台北凹陷及准噶尔盆地南缘中侏罗世煤系为例 . 沉积学报, 2000, 18(4): 585-589.
[19]	王俊玲, 叶连俊, 李伯虎, 陈琪英. 松辽盆地三肇地区榆树林油田葡萄花油层储层沉积模式 . 沉积学报, 1997, 15(1): 37-42.
[20]	李元元, 方少仙, 陈景山. 自然伽玛数字判别法研究沉积微相——以东濮盆地文留地区沙四段为例 . 沉积学报, 1991, 9(4): 59-68.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 1262
HTML全文浏览量: 3
PDF下载量: 1006
被引次数: 0

准噶尔盆地乌尔禾油田高自然伽马砂砾岩特征及其沉积微相研究——以乌36井区百口泉组为例

刊出日期: 2014-08-10

中图分类号: TE121.3⁺2

关键词:

摘要: 基于岩芯编录、测录井资料和薄片分析数据，对准噶尔盆地乌36井区三叠系百口泉组开展了沉积学研究。研究表明，乌36井区百口泉组发育冲积扇沉积体系，扇体内部砂砾岩具有自然伽马异常高的特点，而泥岩具有自然伽马异常低的特点，其原因主要是由于原岩碎屑中富含凝灰岩等高放射性物质，同时沉积物的粒度变化、搬运距离和相带展布控制了砂砾岩自然伽马异常的空间变化，并依据伽马异常的空间变化特点建立了相应的泥质含量计算公式，提出了高自然伽马砂砾岩沉积微相划分的一种新方法。区内主要发育冲积扇扇中辫流线微相、扇中辫流砂岛微相、扇中漫洪带微相和扇缘漫流带微相。精细刻画了各期扇体沉积微相的展布与垂向演化特征，百口泉组三段发育四期扇体，垂向上表现为一个快速水退背景和缓慢水进背景下的沉积演化序列；百口泉组二段发育三期扇体，垂向上表现为退积型演化序列；百口泉组一段则表现为冲积扇扇缘沉积。通过与实际生产对比，本次研究较好地解释了区内生产井的生产状况，验证了利用高自然伽马砂砾岩自然伽马特征研究沉积微相的可行性与实用性。

High GR Glutinite Feature and Micro-Sedimentary Facies in Wuerhe Oil-field, Junggar Basin——Taking the Baikouquan Group in Wu 36 Area as an example

Publish Date: 2014-08-10

Keywords:

Abstract: Based on rock core documentation, well logging analysis and the rock fragment data, we carried out the sedimentology research on the Triassic Baikouquan Group in Wu 36 area of Junggar Basin. This study revealed that the Baikouquan Group developped in alluvial fan system. The glutenite is characterized by unusually high natural gamma and the mudstone is characterized by low inside the alluvial fan. This feature is mainly controlled by the high radioactive substance in the original rock, for example the tuff. The spatial variation in high natural gamma anomaly was influenced by sediment grain size, transport distance and facies distribution. According to the spatial variation characteristics of Gamma anomaly, we established a clay content formula and put forward a new method on the division of sedimentary facies. Our study area mainly develops mid-fan braided stream line microfacies, mid-fan braided stream sand island microfacies, mid-fan sheetflood microfacies and cross flow microfacies in marginal subfacies. We also carefully portrayed the distribution and vertical evolution of these sedimentary microfacies of different stages. The results show that the 3^rdmember in Baikouquan Group developed four fan bodies. There is a sedimentary evolutionary sequence in the vertical profile controlled by fast dereliction and slow retrograding. The 2^nd member in Baikouquan Group developed three fan bodies and presented a retrograding evolutionary sequence in the vertical. The 1^st member in Baikouquan Group performed the alluvial fan marginal sedimentary. Compared with the actual production, this study better explained the production status of the regional producing well and verified the feasibility and practicality of using natural gamma characteristics of high natural gamma glutinite to make research on sedimentary microfacies.

留言板

准噶尔盆地乌尔禾油田高自然伽马砂砾岩特征及其沉积微相研究——以乌36井区百口泉组为例

计量

High GR Glutinite Feature and Micro-Sedimentary Facies in Wuerhe Oil-field, Junggar Basin——Taking the Baikouquan Group in Wu 36 Area as an example

计量

目录

准噶尔盆地乌尔禾油田高自然伽马砂砾岩特征及其沉积微相研究——以乌36井区百口泉组为例

English Abstract

High GR Glutinite Feature and Micro-Sedimentary Facies in Wuerhe Oil-field, Junggar Basin——Taking the Baikouquan Group in Wu 36 Area as an example

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

准噶尔盆地乌尔禾油田高自然伽马砂砾岩特征及其沉积微相研究——以乌36井区百口泉组为例

计量

出版历程

High GR Glutinite Feature and Micro-Sedimentary Facies in Wuerhe Oil-field, Junggar Basin——Taking the Baikouquan Group in Wu 36 Area as an example

计量

出版历程

目录

准噶尔盆地乌尔禾油田高自然伽马砂砾岩特征及其沉积微相研究——以乌36井区百口泉组为例

English Abstract

High GR Glutinite Feature and Micro-Sedimentary Facies in Wuerhe Oil-field, Junggar Basin——Taking the Baikouquan Group in Wu 36 Area as an example

全文HTML

目录

友情链接

期刊在线

联系我们