塔里木盆地顺北地区二叠纪火山活动期次与分布

肖重阳; 杨林; 林波; 尤东华

doi:10.11781/sysydz202002177

塔里木盆地顺北地区二叠纪火山活动期次与分布

doi: 10.11781/sysydz202002177

肖重阳^{1, 2, 3,},
杨林²,
林波²,
尤东华⁴

1.
成都理工大学能源学院, 成都 610059
2.
中国石化西北油田分公司勘探开发研究院, 乌鲁木齐 830011
3.
油气藏地质及开发工程国家重点实验室, 成都 610059
4.
中国石化石油勘探开发研究院无锡石油地质研究所, 江苏无锡 214126

基金项目:

国家“十三五”科技重大专项 2017ZX05005-002

第63批博士后科学基金面上项目 2018M6331865

详细信息

作者简介:
肖重阳(1987-), 男, 博士研究生, 从事沉积储层方面的研究。E-mail: 228236295@qq.com

中图分类号: TE122.2
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- 被引次数: 0
出版历程
- 收稿日期: 2019-07-27
- 修回日期: 2020-02-21
- 刊出日期: 2020-03-28

Volcanic activity stages and distribution during the Permian in the Shunbei area, Tarim Basin

XIAO Chongyang^{1, 2, 3
,},
YANG Lin²,
LIN Bo²,
YOU Donghua⁴

1.
College of Energy, Chengdu University of Technology, Chengdu, Sichuan 610059, China
2.
SINOPEC Northwest Oilfield Branch Company, Urumqi, Xinjiang 830011, China
3.
State Key Laboratory of Oil and Gas Reservoir Geology and Exploration, Chengdu, Sichuan 610059, China
4.
Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

摘要

摘要: 顺北地区位于塔里木盆地中部顺托果勒低隆，该区为玄武岩与英安岩的叠合覆盖区，其二叠系火山岩期次及分布较塔河及塔中地区更难识别。通过对顺北地区27口井中二叠系火山岩的取心观察与采样，并进行薄片鉴定及地球化学元素分析，识别出玄武岩类、安山岩类、英安岩类、凝灰岩类和火山角砾岩类5种基本岩石类型。另外，依据二叠系火山岩的岩性组合与岩电特征对应关系，结合二叠系地震特征将火山活动细分为5个喷发旋回（或期次）：第一期为中酸性火山碎屑岩沉积，以顺北三维区为中心；第二期为基性火山岩，分布主要受古地貌变化影响；第三、四期次火山主要为锥形、盾形中酸性火山熔岩，中间以稳定分布的火山沉积岩层为划分依据；第五期为基性火山熔岩，主要分布于研究区东部。
- 喷发期次 /
- 火山岩 /
- 二叠系 /
- 顺北地区 /
- 塔里木盆地
Abstract: The Shunbei area, located in the Shuntuoguole Low Uplift in the central Tarim Basin, is covered by superimposed basalt and dacite, where volcanic activity stages in the Permian and areal distribution are more difficult to identify compared with those in the Tahe and Tazhong areas. Through core observations and sampling of Permian volcanic rocks from 27 wells in the Shunbei area, we carried out thin section identifications and geochemical element analyses. Five basic rock types were observed, including basalts, andesites, dacites, tuffs and volcanic breccias. In addition, the volcanic activity was subdivided into 5 eruption cycles (or periods) based on the lithology, the petrophysical log characteristics and the seismic characteristics of the Permian section. The first stage was an eruption of intermediate-acid pyroclastic rocks, with the eruption center located in the Shunbei 3D block. The second stage was an eruption of basic volcanic rocks, which was mainly controlled by paleotopo-graphy. The third and fourth stages featured cone-shaped and shield-shaped intermediate-acid volcanic lava, with stable volcanic sediments between the two stages. The fifth stage was an eruption of basic volcanic lava, which mainly distributed in the east of the study area.
- eruption stage /
- volcanic rock /
- Permian /
- Shunbei area /
- Tarim Basin

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图 1 塔里木盆地顺北地区二叠纪火山活动研究区及钻井位置^{[1, 7]}

Figure 1. Volcanic activity areas during Permian and well locations, Shunbei area, Tarim Basin

下载: 全尺寸图片幻灯片

图 2 塔里木盆地顺北地区二叠系火山岩镜下特征

a.X1-5H井，4 415 m，右侧单偏光、左侧正交偏光；辉石玄武岩，斑状结构，基质为长条状斜长石充填柱状及粒状辉石, 见蚀变橄榄石；b.X1-5H井，4 780 m，右侧单偏光、左侧正交偏光；玄武岩，无斑间粒结构，由辉石和斜长石小晶体组成，充填辉石和橄榄石(伊丁石化为红色)；c.X1-5H井，4 430 m，右侧单偏光、左侧正交偏光；安山岩，斑状结构, 基质斜长石辉石、角闪石交织结构；d.X2井，4 530 m，右侧单偏光、左侧正交偏光；杏仁英安岩，斑状结构，绿色为杏仁结构充填绿泥石；e.X5-5H井，4 742.5 m，右侧单偏光、左侧正交偏光；英安岩，斑状结构，斑晶为斜长石及石英，见溶蚀边；f.X1-3井，4 700 m，右侧单偏光、左侧正交偏光；沉凝灰岩，碎屑物质含量大于90%，沉凝灰结构；g.X1-3井，4 725 m，右侧单偏光、左侧正交偏光；流纹质晶屑玻屑凝灰岩，假流动构造；h.X2井，4 848 m，右侧单偏光、左侧正交偏光；岩屑晶屑熔结凝灰岩，假流动构造

Figure 2. Microscopic characteristics of Permian volcanic rocks in Shunbei area, Tarim Basin

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图 3 塔里木盆地顺北地区二叠系火山岩类型TAS图版

图版据Streckeisen^{[5-7, 10-11, 13]}。

Figure 3. TAS map of Permian volcanic rocks in Shunbei area, Tarim Basin

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图 4 塔里木盆地顺北地区二叠系火山期次测井及地震响应特征

Figure 4. Volcanic period logging and seismic response characteristics of Permian in Shunbei area, Tarim Basin

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图 5 塔里木盆地顺北地区二叠系火山岩喷发期次井震对比

Figure 5. Logging and seismic correlation of Permian volcanic rock eruption periods in Shunbei area, Tarim Basin

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表 1 塔里木盆地顺北地区二叠系火成岩主量元素地球化学分析数据

Table 1. Geochemical data of primary elements of Permian igneous rocks in Shunbei area, Tarim Basin %

样品号	深度/m	SiO₂	TiO₂	Al₂O₃	Fe₂O₃	MnO	MgO	CaO	Na₂O	K₂O	P₂O₅	烧失量
X1-3-1	4 530.0	56.42	1.18	14.81	8.09	0.19	2.34	3.73	2.55	3.83	0.16	6.74
X1-3-2	4 580.0	63.95	0.91	14.69	5.33	0.08	1.28	2.33	3.70	2.79	0.33	4.48
X1-3-3	4 700.0	60.31	0.64	15.99	5.85	0.07	1.40	1.72	2.76	3.56	0.15	7.37
X1-5H-1	4 430.0	56.82	1.27	14.86	8.82	0.12	3.74	5.30	2.94	1.63	0.22	4.20
X1-5H-2	4 700.0	60.75	0.78	16.29	6.97	0.11	1.58	1.95	2.82	3.96	0.24	4.36
X1-5H-3	4 760.0	60.29	0.62	13.25	5.49	0.07	1.29	5.41	2.44	4.07	0.17	6.94
X1-5H-4	4 790.0	58.31	1.37	13.08	8.41	0.13	1.98	5.00	2.45	3.26	0.31	5.62
X1-5H-5	4 925.0	59.98	0.57	13.20	5.31	0.06	1.73	5.00	1.89	3.87	0.15	8.09
X2-1	4 847.6	61.09	0.95	14.31	7.49	0.11	0.87	2.75	3.59	4.81	0.53	3.46
X2-2	4 962.4	44.78	3.95	15.23	14.21	0.21	5.68	4.28	3.93	0.91	1.22	5.54
X5-5H-1	4 742.0	59.29	0.56	14.04	6.57	0.10	0.58	2.11	3.22	4.79	0.29	8.45
X5-5H-2	4 742.6	58.10	0.51	12.57	6.75	0.19	0.45	2.22	3.02	4.46	0.29	11.44
X5-5H-3	4 743.0	55.43	0.47	13.26	8.55	0.09	0.54	1.97	3.02	4.45	0.26	11.96
S79-1	4 831.3	58.97	0.98	14.37	6.48	0.09	2.40	2.04	3.06	3.92	0.34	7.35
S79-2	4 864.1	55.34	0.54	14.32	7.15	0.14	1.93	5.99	2.38	3.59	0.28	8.34

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表 2 塔里木盆地顺北地区二叠系岩性测井曲线响应特征数据统计

Table 2. Lithologic log curve response data of Permian in Shunbei area, Tarim Basin

测井曲线	玄武岩		英安岩		凝灰岩		砂岩		火山角砾岩
测井曲线	上段	下段	上段	下段	上段	下段	上段	下段	下段
GR/API	30~40	25~35	110~150	120~170	80~100	80~96	40~55	40~60	65~80
RT/(Ω·m)	10~100	10~100	20~40	20~40	0.8~3	1~7	0.5~2.0	0.5~1.5	1~3
AC/(μs·ft^-1)	50~60	42~55	55~68	50~60	70~85	70~80	85~95	80~92	65~75
DEN/(g·cm^-3)	2.55~2.75	2.60~2.75	2.45~2.55	2.5~2.55	2.28~2.4	2.35~2.55	2.12~2.35	2.15~2.35	2.40~2.55
CNL/%	5~15	5~15	6~10	6~10	25~30	44~124	25~33	15~30	10~20

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表 3 塔里木盆地顺北地区二叠系火山岩活动期次划分特征

Table 3. Classification of Permian volcanic activities in Shunbei area, Tarim Basin

期次	岩性	钻遇井厚度/m	内幕反射特征	顶底界面反射特征	火山岩相
1	火山角砾岩、英安岩	300以下	内幕杂乱、弱反射	强反射波谷	爆发相—火山沉积相
2	玄武岩—凝灰岩组合	120以下	平行板状、弱反射	均为强反射波谷	溢流相—火山沉积相
3	英安岩—凝灰岩组合	350以下	杂乱强反射	顶界面强反射波峰，底界面强反射波谷	溢流相—火山沉积相
4	英安岩—凝灰岩—沉积岩组合	0~400	弱反射、楔形反射	顶界面强反射波峰，底界面强反射波谷	溢流相—火山沉积相
5	玄武岩为主，局部见凝灰岩	50~100	平行板状、强反射	强反射波谷	溢流相

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参考文献(32)

[1]	陈汉林, 杨树锋, 董传万, 等. 塔里木盆地二叠纪基性岩带的确定及大地构造意义[J]. 地球化学, 1997, 26(6): 77-87. doi: 10.3321/j.issn:0379-1726.1997.06.009 CHEN Hanlin, YANG Shufeng, DONG Chuanwan, et al. Confirmation of Permian basite zone in Tarim Basin and its tectonic significance[J]. Geochimica, 1997, 26(6): 77-87. doi: 10.3321/j.issn:0379-1726.1997.06.009
[2]	陈汉林, 杨树锋, 王清华, 等. 塔里木板块早-中二叠世玄武质岩浆作用的沉积响应[J]. 中国地质, 2006, 33(3): 545-552. doi: 10.3969/j.issn.1000-3657.2006.03.010 CHEN Hanlin, YANG Shufeng, WANG Qinghua, et al. Sedimentary response to the Early-Mid Permian basaltic magmatism in the Tarim Plate[J]. Geology in China, 2006, 33(3): 545-552. doi: 10.3969/j.issn.1000-3657.2006.03.010
[3]	刘晓, 关平, 潘文庆, 等. 塔里木盆地二叠系火山岩空间展布的精细刻画及其地质意义[J]. 北京大学学报(自然科学版), 2011, 47(2): 315-320. https://www.cnki.com.cn/Article/CJFDTOTAL-BJDZ201102020.htm LIU Xiao, GUAN Ping, PAN Wenqing, et al. Meticulous characterization of Permian volcanic rocks' spatial distribution and its geological significance in the Tarim Basin[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2011, 47(2): 315-320. https://www.cnki.com.cn/Article/CJFDTOTAL-BJDZ201102020.htm
[4]	闫磊, 李明, 潘文庆. 塔里木盆地二叠纪火成岩分布特征: 基于高精度航磁资料[J]. 地球物理学进展, 2014, 29(4): 1843-1848. https://www.cnki.com.cn/Article/CJFDTOTAL-DQWJ201404048.htm YAN Lei, LI Ming, PAN Wenqing. Distribution characteristics of Permian igneous rock in Tarim Basin: based on the high-precision aeromagnetic data[J]. Progress in Geophysics, 2014, 29(4): 1843-1848. https://www.cnki.com.cn/Article/CJFDTOTAL-DQWJ201404048.htm
[5]	余星, 陈汉林, 杨树锋, 等. 塔里木盆地二叠纪玄武岩的地球化学特征及其与峨眉山大火成岩省的对比[J]. 岩石学报, 2009, 25(6): 1492-1498. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200906020.htm YU Xing, CHEN Hanlin, YANG Shufeng, et al. Geochemical features of Permian basalts in Tarim Basin and compared with Emei-shan LIP[J]. Acta Petrologica Sinica, 2009, 25(6): 1492-1498. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200906020.htm
[6]	厉子龙, 励音骐, 邹思远, 等. 塔里木早二叠世大火成岩省的时空特征和岩浆动力学[J]. 矿物岩石地球化学通报, 2017, 36(3): 418-431. https://www.cnki.com.cn/Article/CJFDTOTAL-KYDH201703006.htm LI Zilong, LI Yinqi, ZOU Siyuan, et al. The temporospatial characteristics and magma dynamics of the Early Permian Tarim large igneous province[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2017, 36(3): 418-431. https://www.cnki.com.cn/Article/CJFDTOTAL-KYDH201703006.htm
[7]	杨树锋, 陈汉林, 厉子龙, 等. 塔里木早二叠世大火成岩省[J]. 中国科学(地球科学), 2014, 44(2): 187-199. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201710004.htm YANG Shufeng, CHEN Hanlin, LI Zilong, et al. Early Permian Tarim large igneous province in Northwest China[J]. Science China (Earth Sciences), 2013, 56(12): 2015-2026. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201710004.htm
[8]	ZHANG Chuanlin, XU Yigang, LI Zhengxiang, et al. Diverse Permian magmatism in the Tarim Block, NW China: genetically linked to the Permian Tarim mantle plume?[J]. Lithos, 2010, 119(3/4): 537-552.
[9]	ZOU Siyuan, LI Zilong, SONG Biao, et al. Zircon U-Pb dating, geochemistry and Sr-Nd-Pb-Hf isotopes of the Wajilitag alkali mafic dikes, and associated diorite and syenitic rocks: implications for magmatic evolution of the Tarim large igneous province[J]. Lithos, 2015, 212/215: 428-442. doi: 10.1016/j.lithos.2014.09.005
[10]	罗静兰, 翟晓先, 蒲仁海, 等. 塔河油田火山岩的层位归属、火山岩岩石学与岩相学特征[J]. 地质科学, 2006, 41(3): 378-391. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200603001.htm LUO Jinglan, ZHAI Xiaoxian, PU Renhai, et al. Horizon, petrology and lithofacies of the volcanic rocks in the Tahe oilfield, northern Tarim Basin[J]. Chinese Journal of Geology, 2006, 41(3): 378-391. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200603001.htm
[11]	朱志新, 王克卓, 郑玉洁, 等. 新疆伊犁地块南缘志留纪和泥盆纪花岗质侵入体锆石SHRIMP定年及其形成时构造背景的初步探讨[J]. 岩石学报, 2006, 22(5): 1193-1200. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200605011.htm ZHU Zhixin, WANG Kezhuo, ZHENG Yujie, et al. Zircon SHRIMP dating of Silurian and Devonian granitic intrusions in the southern Yili block, Xinjiang and preliminary discussion on their tectonic setting[J]. Acta Petrologica Sinica, 2006, 22(5): 1193-1200. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200605011.htm
[12]	朱毅秀, 金之钧, 林畅松, 等. 塔里木盆地塔中地区早二叠世岩浆岩及油气成藏关系[J]. 石油实验地质, 2005, 27(1): 50-54. doi: 10.11781/sysydz200501050 ZHU Yixiu, JIN Zhijun, LIN Changsong, et al. Relations between the Early Permian magmatic rocks and hydrocarbon accumulation in the central Tarim[J]. Petroleum Geology & Experiment, 2005, 27(1): 50-54. doi: 10.11781/sysydz200501050
[13]	刘亚雷, 胡秀芳, 黄智斌, 等. 塔里木盆地塔北隆起西部火山岩⁴⁰Ar-³⁹Ar年代学和地球化学特征[J]. 岩石学报, 2012, 28(8): 2423-2434. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201208012.htm LIU Yalei, HU Xiufang, HUANG Zhibin, et al. ⁴⁰Ar-³⁹Ar geochronology and geochemistry of the volcanic rocks from the west segment of Tabei Uplift, Tarim Basin[J]. Acta Petrologica Sinica, 2012, 28(8): 2423-2434. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201208012.htm
[14]	焦方正. 塔里木盆地顺托果勒地区北东向走滑断裂带的油气勘探意义[J]. 石油与天然气地质, 2017, 38(5): 831-839. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201705001.htm JIAO Fangzheng. Significance of oil and gas exploration in NE strike-slip fault belts in Shuntuoguole area of Tarim Basin[J]. Oil & Gas Geology, 2017, 38(5): 831-839. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201705001.htm
[15]	邓尚, 李慧莉, 张仲培, 等. 塔里木盆地顺北及邻区主干走滑断裂带差异活动特征及其与油气富集的关系[J]. 石油与天然气地质, 2018, 39(5): 878-888. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201805004.htm DENG Shang, LI Huili, ZHANG Zhongpei, et al. Characteristics of differential activities in major strike-slip fault zones and their control on hydrocarbon enrichment in Shunbei area and its surroundings, Tarim Basin[J]. Oil & Gas Geology, 2018, 39(5): 878-888. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201805004.htm
[16]	汤良杰, 黄太柱, 邱海峻, 等. 塔里木盆地塔河地区海西晚期火山岩构造特征与油气成藏[J]. 地质学报, 2012, 86(8): 1188-1197. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201208003.htm TANG Liangjie, HUANG Taizhu, QIU Haijun, et al. The tectonic characteristics and hydrocarbon accumulation of late Hercynian volcanic rocks in the Tahe area, Tarim Basin[J]. Acta Geologica Sinica, 2012, 86(8): 1188-1197. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201208003.htm
[17]	张传林. 塔里木盆地塔中地区火成岩体识别与预测技术[J]. 石油实验地质, 2003, 25(5): 513-516. doi: 10.11781/sysydz200305513 ZHANG Chuanlin. Identification and prediction of volcanic bodies in Tazhong area of the Tarim Basin[J]. Petroleum Geology & Experiment, 2003, 25(5): 513-516. doi: 10.11781/sysydz200305513
[18]	杨金龙, 罗静兰, 何发歧, 等. 塔河地区二叠系火山岩储集层特征[J]. 石油勘探与开发, 2004, 31(4): 44-47. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200404011.htm YANG Jinlong, LUO Jinglan, HE Faqi, et al. Permian volcanic reservoirs in the Tahe region[J]. Petroleum Exploration and Development, 2004, 31(4): 44-47. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200404011.htm
[19]	田军. 塔里木盆地油气勘探成果与勘探方向[J]. 新疆石油地质, 2019, 40(1): 1-10. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD201901002.htm TIAN Jun. Petroleum exploration achievements and future targets of Tarim Basin[J]. Xinjiang Petroleum Geology2019, 40(1): 1-10. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD201901002.htm
[20]	赵锐, 赵腾, 李慧莉, 等. 塔里木盆地顺北油气田断控缝洞型储层特征与主控因素[J]. 特种油气藏, 2019, 26(5): 8-13. https://www.cnki.com.cn/Article/CJFDTOTAL-TZCZ201905002.htm ZHAO Rui, ZHAO Teng, LI Huili, et al. Fault-controlled fracture-cavity reservoir characterization and main-controlling factors in the Shunbei hydrocarbon field of Tarim Basin[J]. Special oil & Gas Reservoirs, 2019, 26(5): 8-13. https://www.cnki.com.cn/Article/CJFDTOTAL-TZCZ201905002.htm
[21]	黄诚. 叠合盆地内部小尺度走滑断裂幕式活动特征及期次判别: 以塔里木盆地顺北地区为例[J]. 石油实验地质, 2019, 41(3): 379-389. doi: 10.11781/sysydz201903379 HUANG Cheng. Multi-stage activity characteristics of small-scale strike-slip faults in superimposed basin and its identification method: a case study of Shunbei area, Tarim Basin[J]. Petroleum Geology & Experiment, 2019, 41(3): 379-389. doi: 10.11781/sysydz201903379
[22]	李曰俊, 孙龙德, 胡世玲, 等. 塔里木盆地塔参1井底部花岗闪长岩的⁴⁰Ar-³⁹Ar年代学研究[J]. 岩石学报, 2003, 19(3): 530-536. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200303018.htm LI Yuejun, SUN Longde, HU Shiling, et al. ⁴⁰Ar-³⁹Ar geochronology of the granite and diorite revealed at the bottom of Tacan 1, the deepest well in China[J]. Acta Petrologica Sinica, 2003, 19(3): 530-536. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200303018.htm
[23]	张洪安, 李曰俊, 吴根耀, 等. 塔里木盆地二叠纪火成岩的同位素年代学[J]. 地质科学, 2009, 44(1): 137-158. ZHANG Hong'an, LI Yuejun, WU Genyao, et al. Isotopic geochronology of Permian igneous rocks in the Tarim Basin[J]. Chinese Journal of Geology, 2009, 44(1): 137-158.
[24]	崔泽宏, 唐跃. 塔河地区海西晚期火山岩地球化学特征及地质意义[J]. 中国地质, 2010, 37(2): 334-346. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201002008.htm CUI Zehong, TANG Yue. Geochemical characteristics and geological significance of Late Hercynian volcanic rocks in Tahe area[J]. Geology in China, 2010, 37(2): 334-346 https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201002008.htm
[25]	HOPSON C, WEN J, TILTON G, et al. Paleozoic Plutonism in east Junggar, Bogdashan, and eastern Tianshan, NW China, EOS[J]. Transactions of the American Geophysical Union, 1989, 70: 1403-1404.
[26]	李彬, 贺凯, 吕海涛, 等. 塔北地区二叠系火山岩岩性特征及油气勘探前景[J]. 石油与天然气地质, 2011, 32(54): 851-858. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201106007.htm LI Bin, HE Kai, LV Haitao, et al. Lithologic characteristics and petroleum exploration potential of the Permian volcanic rocks in northern Tarim Basin[J]. Oil & Gas Geology, 2011, 32(54): 851-858. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201106007.htm
[27]	刘长磊, 张艺琼, 张永, 等. 塔北-塔中区域构造地质大剖面解析及古隆起成因新解[J]. 石油与天然气地质, 2018, 39(5): 1001-1010. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201805015.htm LIU Changlei, ZHANG Yiqiong, ZHANG Yong, et al. Analysis of regional structural cross section of the north and central Tarim Basin and new insights into paleo-uplift origin[J]. Oil & Gas Geology, 2018, 39(5): 1001-1010. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201805015.htm
[28]	JACKSON J A. Glossary of geology[M]. Alexandria: American Geological Institute, 1997.
[29]	张招崇, 王福生, 范蔚茗, 等. 峨眉山玄武岩研究中的一些问题的讨论[J]. 岩石矿物学杂志, 2001, 20(3): 239-246. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200103004.htm ZHANG Zhaochong, WANG Fusheng, FAN Weiming, et al. A discussion on some problems concerning the study of the Emei-shan basalts[J]. Acta Petrologica et Mineralogica, 2001, 20(3): 239-246. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200103004.htm
[30]	徐夕生, 邱检生. 火成岩岩石学[M]. 北京: 科学出版社, 2010. XU Xisheng, QIU Jiansheng. Igneous petrology[M]. Beijing: Science Press, 2010.
[31]	温声明, 王建忠, 王贵重, 等. 塔里木盆地火成岩发育特征及对油气成藏的影响[J]. 石油地球物理勘探, 2005, 40(3): 33-39. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDQ2005S1007.htm WEN Shengming, WANG Jianzhong, WANG Guizhong, et al. The character of the magmatic rock and its influence to the petroleum exploration in the Tarim Basin[J]. Oil Geophysical Prospecting, 2005, 40(3): 33-39. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDQ2005S1007.htm
[32]	朱卡, 李兰斌, 梁浩, 等. 三塘湖盆地石炭系火山岩喷发环境及储层特征研究[J]. 石油天然气学报, 2012, 34(3): 49-54. https://www.cnki.com.cn/Article/CJFDTOTAL-JHSX201203011.htm ZHU Ka, LI Lanbin, LIANG Hao, et al. The eruption environment and reservoir characteristics of carboniferous volcanic rocks in Sangtanghu Basin[J]. Journal of Oil and Gas Technology, 2012, 34(3): 49-54. https://www.cnki.com.cn/Article/CJFDTOTAL-JHSX201203011.htm