Citation: | JIANG Zhibin, HUANG Jiaxuan, LI Yongjun, LI Siyuan, WANG Tao, WANG Jie, PENG Nanhe. 2023. New Evidence on the Stratigraphy and Chronology of 2 140~3 551.63 m Well 424 Section in Karamay Oilfield and “Basin−Mountain” Stratigraphic Comparison. Northwestern Geology, 56(2): 1-9. doi: 10.12401/j.nwg.2022044 |
The establishment and age determination of the stratigraphic sequence in the well is the key evidence for the division and correlation of rock stratigraphic units. This is significant for the correct establishment of the reservoir. The upper section of well 424 (2 140~3 178 m) in Karamay Oilfield is dominated by marine terrestrial clastic rocks. Sporopollen fossils, such as Noeggerathiops−idozonotriletes were obtained in the interbedded dark gray siltstone and gray−black fine sandstone in the depth of 3 176.94~3 178.44 m, indicating that they formed in early to middle stage of Late Carboniferous (Bashkirian−Moscovian); The lower section 3 178~3 551.63 m is mainly composed of volcanic breccia and intercalated lava. LA−ICP−MS zircon U−Pb age of 306 Ma was obtained from the amygdaloidal basaltic andesite at 3 340.50~3 343.50 m. It is considered that the upper terrestrial clastic rocks and the lower volcanic breccia are integrated contact and show obvious dichotomy characteristics. Accordingly, it is confirmed that the upper part (2 140~3 178 m) of the well 424 is comparable to the lower part of the stratotype section of the Aladeyikesai Formation in the Hala’alate Mountain, and the lower part (3 178~3 551.63 m) is comparable to the upper part of the Hala’alate Formation. This result not only subdivides lithostratigraphic unit of Well 424, but also makes up the deficiency of the unclear original stratigraphic contact relationship and old−new relationship between the stratotype sections of Aladeyikesai and Hala’alate formations in the mountain area.
陈江新,徐倩,李永军,等. 车排子地区车47井石炭系划分及对比[J]. 新疆石油地质,2022,43(4):410–416. |
江汝锋. 克拉玛依油田石炭系火山岩区断裂特征与油气成藏关系[D]. 东营: 中国石油大学(华东), 2014 JIANG Rufeng, The Relationship between Fault Characteristics and Petroleum Accumulation of Carboniferous Volcanic in Karamay Oilfield[D]. Dongying: China University of Petroleum (East China), 2014 |
靳军,王剑,刘金,等. 准噶尔盆地克—百断裂带石炭系深部岩性岩相及时空分布特征[J]. 西北大学学报(自然科学版),2018,48(02):238–245. doi: 10.16152/j.cnki.xdxbzr.2018-02-013 |
李甘雨,李永军,王冉,等. 西准噶尔哈拉阿拉特山一带晚石炭世赞岐岩的发现及其地质意义[J]. 岩石学报,2017,33(1):16–30. |
李甘雨,李永军,向坤鹏,等. 西准噶尔哈拉阿拉特组的重新厘定及区域对比[J]. 地层学杂志,2016,40(1):76–84. doi: 10.19839/j.cnki.dcxzz.2016.01.009 |
李永军, 李卫东, 杨高学, 等. 新疆东西准噶尔泥盆系-石炭系建组剖面及区域对比[M]. 北京: 地质出版社, 2021: 163−291 LI Yongjun, LI Weidong, YANG Gaoxue, et al. Devonian-Carboniferous Stratotype Sections and Regional Correlation in Eastern and Western Junggar, Xinjiang[M]. Beijing: Geological Publishing House, 2021: 163−291. |
李永军,徐倩,杨高学,等. 陆内“滞后”弧岩浆岩及其地质意义—来自西准噶尔乌尔禾北早二叠世岩浆作用的证据[J]. 地学前缘,2016a,23(4):190–199. |
李永军,徐倩,刘佳,等. 新疆西准噶尔哈山地区佳木河组的重新厘定及地质意义[J]. 地球科学,2016b,41(9):1479–1488. |
李永军,佟丽莉,张兵,等. 论西准噶尔石炭系希贝库拉斯组与包古图组的新老关系[J]. 新疆地质,2010,28(02):130–136. doi: 10.3969/j.issn.1000-8845.2010.02.003 |
潘虹,李晓山,钱川川,等. 准噶尔盆地克百断裂带石炭系内幕型火山岩储层特征及成藏规律[J]. 东北石油大学学报,2022,46(01):62–75+122+9−10. doi: 10.3969/j.issn.2095-4107.2022.01.006 |
孙羽,李永军,佟丽莉,等. 西准噶尔希贝库拉斯组整合于包古图组之上的确认[J]. 新疆地质,2014,32(02):153–157. |
王韬,徐倩,李永军,等. 车排子油田南部火山岩地质时代及成因[J]. 新疆石油地质,2022,43(2):160–168. |
王玉净,金玉玕,江纳言. 论哈拉阿拉特组的时代及古环境特征[J]. 地层学杂志,1987,11(01):53–57. doi: 10.19839/j.cnki.dcxzz.1987.01.006 |
吴元保,郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报,2004,49(16):1589–1604. doi: 10.3321/j.issn:0023-074X.2004.16.002 |
向坤鹏,李永军,李钊,等. 新疆西准噶尔哈拉阿拉特山火山岩LA ICP-MS锆石U-Pb年龄、地球化学特征及意义[J]. 地质学报,2015a,89(05):843–855. doi: 10.3969/j.issn.0001-5717.2015.05.002 |
向坤鹏. 新疆西准噶尔包古图-哈拉阿拉特山一带石炭纪沉积盆地分析及构造意义[D]. 西安: 长安大学, 2015b XIANG Kunpeng, Carboniferous Sedimentary Basin Analysis and Tectonic Significance in the Baogutu-Hala’alate Mountain, Western Junggar, Xinjiang[D]. Xi’an: Chang’an University, 2015b. |
张璐瑾. 新疆克拉玛依地区佳木河组若干重要孢粉类型[J]. 微体古生物学报, 2003, 20(4): 7 ZHANG Lujin, Some important palynomorphs from the jiamuhe formation of the karamay region, xinjiang[J]. Acta Micropalaeontologica Sinica, 2003, 20(4): 7 |
Geological structure map of the Karamay oilfield
Comprehensive stratigraphic histogram of core in well section 2 140~3 551.63 m of well 424
Photo of geological characteristics of core of well 424
Photo of 424 well spore powder samples, Karamay Oilfield
Core and microscopic characteristics of amygdaloidal basaltic andesite samples
Representative zircon CL image and U–Pb age map of basalt in well 424