鄂尔多斯盆地渭北隆起带重磁场特征Characteristics of gravity and magnetic field in Weibei uplift of Ordos basin
许文强,袁炳强,张春灌,张波,许海红,马小雷
XU Wenqiang,YUAN Bingqiang,ZHANG Chunguan,ZHANG Bo,XU Haihong,MA Xiaolei
摘要(Abstract):
通过对研究区已有重、磁测量资料的整理和研究,结合钻井、地质、电法及地震等成果,讨论了重磁异常分布特征,具此推断断裂构造,划分研究区的构造单元,预测油页岩有利区。研究结果表明,鄂尔多斯盆地渭北隆起地重磁场具有"东高西低、中间高南北低、高低相间"的基本特征;主断裂呈北东向展布,近东西向和北西向等次级断裂切断了主断裂,形成了"多"字形分布的构造特征;根据重磁场特征在南北向和东西向上的显著差异,渭北隆起带可划分为宜君-黄龙断坡带、土桥-照金断褶带、彬县-灵台褶皱带、麟游-永寿褶皱带、耀县-澄城断褶带和合阳-澄城断隆带6个构造单元。宜君-黄龙断坡带和耀县-澄城断褶带三叠系面积广、分布稳定、沉积厚度大、烃源岩丰富,是寻找三叠系延长组油页岩层勘探目标的有利带。
This paper neatened and studied the gravity and magnetic measurement data in the study area. It used these data in combination with drilling, geological, electrical and seisimic results in the study area.The distribution of gravity and magnetic anomalies have been discussed, the faulting structures have been speculated, the tectonic units of the study area have been divided and the favourable areas for oil shale have also been predicted.The results showed that gravity and magnetic fields have the following basic features: "high in the east and low in the west, high in the center and low in the south and the north, the high and the low are alternated".The main fault of the study area is NE-trending.Nearly EW and NW-trending secondary faults cut off the main fault, forming "多"-shaped tectonic features.According to significant differences on north-south and east-west, Weibei uplift can be divided into 6 tectonic units, such as Yijun-Huanglong ramp zone, Tuqiao-Zhaojin fault fold belt, Bin county-Lingtai fold belt, Linyou-Yong shou fold belt, Yao county-Chengcheng fault-fold belt, Heyang-Chengcheng fault-uplift belt. Trissic in Yi jun-Huanglong ramp zone and Yao county-Chengcheng fault-fold belt has wide area, distributional stability, large sedimentary thickness and hydrocarbin source rocks. They may be favourable exploration target zones for Triassic Yanchang Formation in the study area.
关键词(KeyWords):
油页岩有利区;断裂构造;重磁场特征;渭北隆起;鄂尔多斯盆地
favourable areas for oil shale;faulting structure;gravity and magnetic field features;Weibei uplift;Ordos basin
基金项目(Foundation): 中国地质调查局资源调查与评价项目(12120113040300-03);; 陕西省教育厅专项科研计划项目(14KJ1579);; 西安石油大学研究生创新基金项目(2014cx130220)
作者(Author):
许文强,袁炳强,张春灌,张波,许海红,马小雷
XU Wenqiang,YUAN Bingqiang,ZHANG Chunguan,ZHANG Bo,XU Haihong,MA Xiaolei
参考文献(References):
- [1]杨俊杰,裴锡古.中国天然气地质学(卷四)[M].北京:石油工业出版社,1996:4–18.
- [2]高飞.渭北地区中新生代构造特征及其演化和改造[D].西安:西北大学,2009.
- [3]周正.鄂尔多斯盆地南缘构造特征研究[D].西安:西北大学,2009.
- [4]时建超.鄂尔多斯南缘中新生代构造特征及演化[D].西安:西北大学,2010.
- [5]王建强.鄂尔多斯盆地南部中新生代演化-改造及盆山耦合关系[D].西安:西北大学,2010.
- [6]贾进斗,何国琦,李茂松.鄂尔多斯盆地基底结构特征及其对古生界天然气的控制[J].高校地质学报,1997,3(2):144–153.
- [7]马润勇,朱浩平,张道法,等.鄂尔多斯盆地基底断裂及其现代活动性[J].地球科学与环境学报,2009,31(4):400–408.
- [8]何紫娟.重磁综合处理解释在鄂尔多斯区域构造中的应用研究[D].北京:中国地质大学,2013.
- [9]张静.鄂尔多斯盆地南部铜川组油页岩成因及资源潜力研究[D].西安:长安大学,2010.
- [10]骆垠山,张哨楠,张枝焕,等.鄂尔多斯盆地南部油页岩矿有利勘探区预测[J].中国矿业,2014,23(1):83–85.
- [11]昌燕,刘人和,拜文华,等.鄂尔多斯盆地南部三叠系油页岩地质特征及富集律[J].中国石油勘探,2012(2):74–78.
- [12]邓南涛,张枝焕,任来义,等.鄂尔多斯盆地南部延长组油页岩地球化学特征及分布规律[J].石油实验地质,2013,35(4):432–437.
- [13]李玉宏,李金超,姜亭,等.鄂尔多斯盆地何家坊地区三叠系油页岩特征[J].吉林大学学报:地球科学版,2009(1):65–71.
- [14]卢进才,李玉宏,魏仙样,等.鄂尔多斯盆地三叠系延长组长7油层组油页岩沉积环境与资源潜力研究[J].吉林大学学报:地球科学版,2006(6):928–932.
- [15]任隽.渭河盆地深部地壳结构探测与盆地构造研究[D].西安:长安大学,2012.
文章评论(Comment):
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- 油页岩有利区
- 断裂构造
- 重磁场特征
- 渭北隆起
- 鄂尔多斯盆地
favourable areas for oil shale - faulting structure
- gravity and magnetic field features
- Weibei uplift
- Ordos basin