华北克拉通胶莱盆地马山地区粗面英安岩磷灰石U-Pb年代学及其地质意义

doi:10.19657/j.geoscience.1000-8527.2023.053

现代地质 ›› 2024, Vol. 38 ›› Issue (01): 117-127.DOI: 10.19657/j.geoscience.1000-8527.2023.053

• 矿物学、岩石学、矿床学 • 上一篇下一篇

华北克拉通胶莱盆地马山地区粗面英安岩磷灰石U-Pb年代学及其地质意义

朱拓¹^,²^,³(), 何登洋¹^,²^,³, 黄雅琪¹^,²^,³, 邱昆峰¹^,²^,³()

1.中国地质大学(北京)地球科学与资源学院,北京 100083
2.中国地质大学地质过程与矿产资源国家重点实验室,北京 100083
3.中国地质大学(北京)深时数字地球前沿科学中心,北京 100083

收稿日期:2022-12-13 修回日期:2023-11-27 出版日期:2024-02-10 发布日期:2024-03-20
通讯作者: 邱昆峰,男,博士生导师,教授,1986年出生,矿床学专业,主要从事矿床学研究工作。Email:kunfengqiu@qq.com
作者简介:朱拓,男,本科生,2002年出生,地质学专业,主要从事岩石学与地球化学相关工作。Email:tuo.zhu@qq.com。
基金资助:
国家自然科学基金项目(42261134535);中国地质大学(北京)创新创业训练计划项目(S202211415007);山东省深部金矿探测大数据应用开发工程实验室项目(SDK202211);山东省深部金矿探测大数据应用开发工程实验室项目(SDK202214);深时数字地球前沿科学中心项目(2652023001);高等学校学科创新引智计划项目(BP0719021)

Apatite U-Pb Geochronology of the Trachy Dacite in Mashan Area, Jiaolai Basin, North China Craton, and Its Geological Significance

ZHU Tuo¹^,²^,³(), HE Dengyang¹^,²^,³, HUANG Yaqi¹^,²^,³, QIU Kunfeng¹^,²^,³()

1. School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China
2. State Key Laboratory of Geological Processes and Mineral Resources, Beijing 100083, China
3. Frontiers Science Center for Deep-time Digital Earth, China University of Geosciences (Beijing), Beijing 100083, China

Received:2022-12-13 Revised:2023-11-27 Online:2024-02-10 Published:2024-03-20

摘要/Abstract

摘要：

五莲—青岛—烟台断裂是胶莱盆地重要的控盆断裂之一,控制了盆地的形成与演化,主要由牟平—即墨断裂和桃村断裂等多条NNE向断裂组成。前人研究表明,五莲—青岛—烟台断裂运动学转换历史先后可划分为晚侏罗世左旋走滑、早白垩世伸展断陷和晚白垩世—古新世右旋走滑三个阶段,但其新生代右旋走滑事件的持续时间仍存在争议。已有研究表明,区域上同尺度断裂走滑运动温度为550~650 ℃,显著高于磷灰石U-Pb体系封闭温度(350~550 ℃),因此磷灰石可能是记录五莲—青岛—烟台断裂右旋走滑的理想对象。本文选取胶莱盆地马山粗面英安岩中的磷灰石进行U-Pb年代学研究,拟约束五莲—青岛—烟台断裂的右旋走滑持续时间。磷灰石U-Pb年龄为(64.1±3.7) Ma,明显晚于早白垩世寄主粗面英安岩锆石U-Pb年龄(119.3±1.6) Ma,表明自早白垩世以来磷灰石至少经历了一次热事件导致其U-Pb同位素体系重置。早白垩世以来,由于印度板块和欧亚板块的碰撞,以及古太平洋板块由NWW向俯冲转变为NW向俯冲,导致了古新世胶莱盆地N—S向拉分和牟平—即墨断裂右旋走滑。因此,本文认为马山粗面英安岩磷灰石U-Pb年龄记录了五莲—青岛—烟台断裂右旋走滑热事件,表明其右旋走滑可能持续到古新世。

关键词: 磷灰石U-Pb年代学, 粗面英安岩, 五莲—青岛—烟台断裂, 古新世右旋走滑

Abstract:

The Wulian-Qingdao-Yantai fault (WQYF) is one of the most important basin-controlling faults in the Jiaolai basin, where the fault dominates the formation and evolution of the basin.This fault is mainly composed of abundant NNE faults, such as Muping-Jimo fault and Taocun fault.The WQYF experienced sinistral strike-slip movement in Late Jurassic, extensional rift in Early Cretaceous, and dextral strike-slip movement during Late Cretaceous-Paleocene.However, the most key question that the duration of the Cenozoic dextral strike-slip movement still remains unclear.Previous studies suggested that temperature of strike-slip movement in this region is about 550-650 ℃, which is higher than the closure temperature, 350-550 ℃, of the apatite U-Pb system.Therefore, in this case apatite can be an ideal candidate to investigate the dextral strike-slip of the WQYF.In this study, we conducted U-Pb dating of apatite from the Early Cretaceous trachy-dacite in the Mashan area and obtained the U-Pb age of 64.1±3.7 Ma.The measured magmatic age of apatite is different from the crystallization age of the Mashan trachy-dacite, indicating that at least there was one geothermal event which reset the apatite U-Pb isotope system in Early Paleocene.Since Early Cretaceous, the collision between the Indian plate and Eurasian plate, and the switch of subduction direction of the paleo-Pacific plate from NWW to NW result in a north-south extension of the Jiaolai basin and the dextral strike-slip of the Muping-Jimo fault.Therefore, we propose that the apatite U-Pb age of the Mashan trachy-dacite documented the dextral strike-slip thermal event of the WQYF, and indicates that the dextral strike-slip may continue until Paleocene.

Key words: apatite U-Pb geochronology, trachy-dacite, Wulian-Qingdao-Yantai fault, Paleocene dextral strike-slip

中图分类号:

P597

朱拓, 何登洋, 黄雅琪, 邱昆峰. 华北克拉通胶莱盆地马山地区粗面英安岩磷灰石U-Pb年代学及其地质意义[J]. 现代地质, 2024, 38(01): 117-127.

ZHU Tuo, HE Dengyang, HUANG Yaqi, QIU Kunfeng. Apatite U-Pb Geochronology of the Trachy Dacite in Mashan Area, Jiaolai Basin, North China Craton, and Its Geological Significance[J]. Geoscience, 2024, 38(01): 117-127.

图/表 7

参考文献 69

[1]	索艳慧, 李三忠, 曹现志, 等. 中国东部中新生代反转构造及其记录的大洋板块俯冲过程[J]. 地学前缘, 2017, 24(4): 249-267. DOI
[2]	ZHAI M G, ZHU R X, LIU J M, et al. Time range of Mesozoic tectonic regime inversion in eastern North China Block[J]. Science in China (Series D: Earth Sciences), 2004, 47(2): 151-159.
[3]	ZHANG Y Q, DONG S W, SHI W. Cretaceous deformation history of the middle Tan-Lu fault zone in Shandong Province, Eastern China[J]. Tectonophysics, 2003, 363(3/4): 243-258. DOI URL
[4]	TANG J, ZHENG Y F, WU Y B, et al. Zircon U-Pb age and geochemical constraints on the tectonic affinity of the Jiaodong terrane in the Sulu orogen, China[J]. Precambrian Research, 2008, 161(3/4): 389-418. DOI URL
[5]	张岳桥, 李金良, 张田, 等. 胶东半岛牟平—即墨断裂带晚中生代运动学转换历史[J]. 地质论评, 2007, 53(3): 289-300.
[6]	刘凤, 栾锡武. 桃村断裂在北黄海盆地的延伸问题探讨[M]. 合肥: 中国科学技术大学出版社, 2009.
[7]	周本刚, 冉勇康, 环文林, 等. 山东海阳断裂东石兰沟段晚更新世以来地表断错特征与最大潜在地震估计[J]. 地震地质, 2002, 24(2): 159-166.
[8]	戴俊生, 陆克政, 宋全友, 等. 胶莱盆地的运动学特征[J]. 石油大学学报(自然科学版), 1995, 19(2): 1-6.
[9]	WATSON E B, HARRISON T M, RYERSON F J. Diffusion of Sm,Sr, and Pb in fluorapatite[J]. Geochimica et Cosmochi-mica Acta, 1985, 49(8): 1813-1823.
[10]	CHERNIAK D J, LANFORD W A, RYERSON F J. Lead diffusion in apatite and zircon using ion implantation and Rutherford Backscattering techniques[J]. Geochimica et Cosmochimica Acta, 1991, 55(6): 1663-1673. DOI URL
[11]	SMYE A J, MARSH J H, VERMEESCH P, et al. Applications and limitations of U-Pb thermochronology to middle and lower crustal thermal histories[J]. Chemical Geology, 2018, 494: 1-18. DOI URL
[12]	RIBEIRO B V, LAGOEIRO L, FALEIROS F M, et al. Strain localization and fluid-assisted deformation in apatite and its influence on trace elements and U-Pb systematics[J]. Earth and Planetary Science Letters, 2020, 545: 116421. DOI URL
[13]	NAKANO T, AWAZU T, UMAKOSHI Y. Plastic deformation and operative slip system in mineral fluorapatite single crystal[J]. Scripta Materialia, 2001, 44(5): 811-815. DOI URL
[14]	SAKA H, GOTO D, MOON W. Dislocations in plastically deformed apatite[J]. Journal of Materials Science, 2008, 43(9): 3234-3239. DOI URL
[15]	HARLOV D E. Apatite: A fingerprint for metasomatic processes[J]. Elements, 2015, 11(3): 171-176. DOI URL
[16]	王微, 宋传中, 李加好, 等. 郯庐断裂带肥东桃源韧性剪切带构造分析及时限探究[J]. 地质科学, 2016, 51(4): 1040-1058.
[17]	孙晓猛, 刘永江, 孙庆春, 等. 敦密断裂带走滑运动的⁴⁰Ar/³⁹Ar年代学证据[J]. 吉林大学学报(地球科学版), 2008, 38(6): 965-972.
[18]	TANG J, ZHENG Y F, WU Y B, et al. Geochronology and geochemistry of metamorphic rocks in the Jiaobei terrane: Constraints on its tectonic affinity in the Sulu orogen[J]. Precambrian Research, 2007, 152(1/2): 48-82. DOI URL
[19]	XIE S W, WU Y B, ZHANG Z M, et al. U-Pb ages and trace elements of detrital zircons from Early Cretaceous sedimentary rocks in the Jiaolai Basin, north margin of the Sulu UHP terrane: Provenances and tectonic implications[J]. Lithos, 2012, 154: 346-360. DOI URL
[20]	DENG J, YANG L Q, LI R H, et al. Regional structural control on the distribution of world-class gold deposits: An overview from the Giant Jiaodong Gold Province, China[J]. Geological Journal, 2019, 54(1): 378-391. DOI URL
[21]	LI S Z, ZHAO G C, DAI L M, et al. Mesozoic Basins in Eastern China and their bearing on the deconstruction of the North China Craton[J]. Journal of Asian Earth Sciences, 2012, 47: 64-79. DOI URL
[22]	李金良, 张岳桥, 柳宗泉, 等. 胶莱盆地沉积-沉降史分析与构造演化[J]. 中国地质, 2007, 34(2): 240-250.
[23]	DENG J, WANG C M, BAGAS L, et al. Cretaceous-Cenozoic tectonic history of the Jiaojia Fault and gold mineralization in the Jiaodong Peninsula, China: Constraints from zircon U-Pb, illite K-Ar, and apatite fission track thermochronometry[J]. Mineralium Deposita, 2015, 50(8): 987-1006. DOI URL
[24]	YANG Q Y, SANTOSH M, SHEN J F, et al. Juvenile vs.recycled crust in NE China: Zircon U-Pb geochronology, Hf isotope and an integrated model for Mesozoic gold mineralization in the Jiaodong Peninsula[J]. Gondwana Research, 2014, 25(4): 1445-1468. DOI URL
[25]	郭云成, 段留安, 韩小梦, 等. 胶东前垂柳金矿区花岗岩锆石U-Pb年代学和地球化学特征及其地质意义[J]. 现代地质, 2022, 36(3): 876-897.
[26]	高建伟, 赵国春, 毛小红, 等. 山东乳山金青顶金矿成矿构造和应力场研究[J]. 现代地质, 2011, 25(6): 1099-1107.
[27]	李秀章, 王立功, 李衣鑫, 等. 胶东艾山岩体二长花岗岩地球化学、锆石U-Pb年代学及Lu-Hf同位素特征研究[J]. 现代地质, 2022, 36(1): 333-346.
[28]	张华全, 张维昕, 李洪杰. 山东胶莱盆地金矿成矿条件及找矿方向[J]. 黄金科学技术, 2008, 16(2): 12-17, 23.
[29]	付文钊. 胶莱盆地白垩纪层序地层与盆地演化过程研究[D]. 青岛: 山东科技大学, 2014.
[30]	佟彦明. 胶莱盆地构造演化研究[D]. 武汉: 中国地质大学, 2007.
[31]	曹光跃, 薛怀民, 刘哲, 等. 鲁西临朐地区早白垩世青山群火山岩的年代学、地球化学及岩石成因[J]. 地质学报, 2018, 92(3): 503-519.
[32]	张岳桥, 李金良, 张田, 等. 胶莱盆地及其邻区白垩纪—古新世沉积构造演化历史及其区域动力学意义[J]. 地质学报, 2008, 82(9): 1229-1257.
[33]	NI J L, LIU J L, TANG X L, et al. The Wulian metamorphic core complex: A newly discovered metamorphic core complex along the Sulu orogenic belt, Eastern China[J]. Journal of Earth Science, 2013, 24(3): 297-313. DOI URL
[34]	LI S Z, ZHAO G C, DAI L M, et al. Cenozoic faulting of the Bohai Bay Basin and its bearing on the destruction of the eastern North China Craton[J]. Journal of Asian Earth Sciences, 2012, 47: 80-93. DOI URL
[35]	LAN H Y, LI S Z, LI X Y, et al. Early Mesozoic intracontinental deformation in the eastern North China Block: Implication for an indentation model of North China to South China blocks[J]. Geological Journal, 2017, 52(Suppl): 8-21. DOI URL
[36]	李三忠, 索艳慧, 李玺瑶, 等. 西太平洋中生代板块俯冲过程与东亚洋陆过渡带构造-岩浆响应[J]. 科学通报, 2018, 63(16): 1550-1593.
[37]	BARFOD G H, KROGSTAD E J, FREI R, et al. Lu-Hf and PbSL geochronology of apatites from Proterozoic terranes: A first look at Lu-Hf isotopic closure in metamorphic apatite[J]. Geochimica et Cosmochimica Acta, 2005, 69(7): 1847-1859. DOI URL
[38]	LIU Y S, GAO S, HU Z C, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the trans-north China orogen: U-Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths[J]. Journal of Petrology, 2010, 51(1/2): 537-571. DOI URL
[39]	ANDERSEN T. Correction of common lead in U-Pb analyses that do not report ²⁰⁴Pb[J]. Chemical Geology, 2002, 192(1/2): 59-79. DOI URL
[40]	YU H C, QIU K F, NASSIF M T, et al. Early orogenic gold mineralization event in the West Qinling related to closure of the Paleo-Tethys Ocean-Constraints from the Ludousou gold deposit, central China[J]. Ore Geology Reviews, 2020, 117: 103217. DOI URL
[41]	STRECK M J. Mineral textures and zoning as evidence for open system processes[J]. Reviews in Mineralogy and Geochemistry, 2008, 69(1): 595-622. DOI URL
[42]	LADENBURGER S, MARKS M A W, UPTON B, et al. Compositional variation of apatite from rift-related alkaline igneous rocks of the Gardar Province, South Greenland[J]. American Minera-logist, 2016, 101(3): 612-626.
[43]	KRNETA S, CIOBANU C L, COOK N J, et al. Apatite at Olympic Dam, South Australia: A petrogenetic tool[J]. Lithos, 2016, 262: 470-485. DOI URL
[44]	DENG J, WANG Q F, LIU X F, et al. The formation of the Jiaodong gold Province[J]. Acta Geologica Sinica, 2022, 96(6): 1801-1820. DOI URL
[45]	QIU K F, DENG J, SAI S X, et al. Low-temperature thermochronology for defining the tectonic controls on heterogeneous gold endowment across the Jiaodong peninsula, eastern China[J]. Tectonics, 2023, 42(1): e2022TC007669.
[46]	DENG J, YANG L Q, GROVES D I, et al. An integrated mineral system model for the gold deposits of the giant Jiaodong Province, Eastern China[J]. Earth-Science Reviews, 2020, 208: 103274. DOI URL
[47]	何登洋, 邱昆峰, 于皓丞, 等. 华北克拉通胶莱盆地马山地区早白垩世粗面英安岩岩石成因[J]. 岩石学报, 2020, 36(12): 3705-3720.
[48]	丁正江, 孙丰月, 刘福来, 等. 胶东中生代动力学演化及主要金属矿床成矿系列[J]. 岩石学报, 2015, 31(10): 3045-3080.
[49]	邱连贵, 任凤楼, 曹忠祥, 等. 胶东地区晚中生代岩浆活动及对大地构造的制约[J]. 大地构造与成矿学, 2008, 32(1): 117-123.
[50]	苗来成, 罗镇宽, 关康, 等. 玲珑花岗岩中锆石的离子质谱U-Pb年龄及其岩石学意义[J]. 岩石学报, 1998, 14(2): 198-206.
[51]	徐洪林, 张德全, 孙桂英. 胶东昆嵛山花岗岩的特征、成因及其与金矿的关系[J]. 岩石矿物学杂志, 1997, 16(2): 131-143.
[52]	郭敬辉, 陈福坤, 张晓曼, 等. 苏鲁超高压带北部中生代岩浆侵入活动与同碰撞—碰撞后构造过程: 锆石 U-Pb 年代学[J]. 岩石学报, 2005, 21(4): 1281-1301.
[53]	张田, 张岳桥. 胶北隆起晚中生代构造-岩浆演化历史[J]. 地质学报, 2008, 82(9): 1210-1228.
[54]	胡世玲, 王松山, 桑海清, 等. 山东玲珑和郭家岭岩体的同位素年龄及其地质意义[J]. 岩石学报, 1987, 3(3):83-89.
[55]	周建波, 郑永飞, 赵子福. 山东五莲中生代岩浆岩的锆石U-Pb年龄[J]. 高校地质学报, 2003, 9(2): 185-194.
[56]	谭俊, 魏俊浩, 杨春福, 等. 胶东郭城地区脉岩类岩石地球化学特征及成岩构造背景[J]. 地质学报, 2006, 80(8): 1177-1188.
[57]	张宏福, 英基丰, 汤艳杰, 等. 华北东部中、新生代岩石圈地幔的不均一性: 来自橄榄石的组成填图结果[J]. 岩石学报, 2006, 22(9): 2279-2288.
[58]	孟繁聪, 李天福, 薛怀民, 等. 胶莱盆地晚白垩世不同地幔源区的两种基性岩浆: 诸城玄武岩和胶州玄武岩的对比[J]. 岩石学报, 2006, 22(6): 1644-1656.
[59]	邱检生, 王德滋, 罗清华, 等. 鲁东胶莱盆地青山组火山岩的⁴⁰Ar-³⁹Ar定年: 以五莲分岭山火山机构为例[J]. 高校地质学报, 2001, 7(3): 351-355.
[60]	FAN W M, ZHANG H F, BAKER J, et al. On and off the North China Craton: Where is the Archaean keel?[J]. Journal of Petrology, 2000, 41(7): 933-950. DOI URL
[61]	RUDNICK R L, GAO S, LING W L, et al. Petrology and geochemistry of spinel peridotite xenoliths from Hannuoba and Qixia, North China Craton[J]. Lithos, 2004, 77(1/2/3/4): 609-637. DOI URL
[62]	QIU K F, DENG J, LAFLAMME C, et al. Giant Mesozoic gold ores derived from subducted oceanic slab and overlying sediments[J]. Geochimica et Cosmochimica Acta, 2023, 343: 133-141. DOI URL
[63]	唐华风, 程日辉, 白云风, 等. 胶莱盆地构造演化规律[J]. 世界地质, 2003, 22(3): 246-251.
[64]	施炜, 张岳桥, 董树文, 等. 山东胶莱盆地构造变形及形成演化: 以王氏群和大盛群变形分析为例[J]. 地质通报, 2003, 22(5): 325-334.
[65]	任凤楼, 张岳桥, 邱连贵, 等. 胶莱盆地白垩纪构造应力场与转换机制[J]. 大地构造与成矿学, 2007, 31(2): 157-167.
[66]	MARUYAMA S, ISOZAKI Y, KIMURA G, et al. Paleogeographic maps of the Japanese Islands: Plate tectonic synthesis from 750Ma to the present[J]. Island Arc, 1997, 6(1): 121-142. DOI URL
[67]	翟慎德. 胶莱盆地莱阳凹陷构造特征及演化[J]. 石油实验地质, 2003, 25(2): 137-142.
[68]	CHARLES N, AUGIER R, GUMIAUX C, et al. Timing, duration and role of magmatism in wide rift systems: Insights from theJiaodong Peninsula (China, East Asia)[J]. Gondwana Research, 2013, 24(1): 412-428. DOI URL
[69]	DENG J, QIU K F, WANG Q F, et al. In situ dating of hydrothermal monazite and implications for the geodynamic controls on ore formation in the Jiaodong gold Province, eastern China[J]. Economic Geology, 2020, 115(3): 671-685. DOI URL

测点号	Th	U	Th/U	²⁰⁷Pb/²⁰⁶Pb			²⁰⁶Pb/²³⁸U			测点号	Th	U	Th/U	²⁰⁷Pb/²⁰⁶Pb		²⁰⁶Pb/²³⁸U
测点号	(10^-6)		Th/U	比值	1σ		比值		1σ	测点号	(10^-6)		Th/U	比值	1σ	比值	1σ
17MS01.2	1270	1181	1.08	0.5207	3.0654	49.087		1.8747		17MS01.35	464	472	0.98	0.8951	1.4044	1.3221	1.8974
17MS01.3	6878	249	27.66	0.891	1.2942	3.0512		4.23195		17MS01.37	123	25	4.93	0.5263	4.0704	39.6814	2.5101
17MS01.5	61	7	8.57	0.8688	1.2268	2.5613		1.1505		17MS01.38	1362	136	10.01	0.8535	1.3220	2.5465	4.5574
17MS01.6	1644	187	8.81	0.8868	1.3172	2.5214		1.7101		17MS01.39	56	16	3.37	0.8497	1.0897	2.7783	1.1734
17MS01.7	106	22	4.88	0.8586	1.2233	4.5204		1.2678		17MS01.40	5	17	0.28	0.8740	1.2181	1.0480	1.9597
17MS01.8	86	13	6.91	0.8760	1.1689	2.4897		1.3219		17MS01.42	196	30	6.50	0.8243	2.5830	0.6932	4.8606
17MS01.9	79	16	5.09	0.9095	1.1094	1.2497		2.1105		17MS01.43	59	7	8.42	0.9094	0.8948	0.1111	11.2151
17MS01.10	76	14	5.30	0.8834	1.5750	2.9378		1.5872		17MS01.44	192	52	3.69	0.5016	2.0304	44.7253	1.9601
17MS01.12	94	14	6.60	0.8743	1.4404	1.9390		1.5487		17MS01.45	1391	1995	0.70	0.6291	3.7503	30.8625	2.4905
17MS01.13	463	462	1.00	0.8804	1.3690	1.6412		1.3879		17MS01.46	1274	1874	0.68	0.5888	3.5811	35.6714	2.1179
17MS01.14	453	461	0.98	0.4845	3.3717	45.5478		2.3638		17MS01.47	6466	381	16.96	0.9039	1.4358	2.2080	3.0184
17MS01.16	155	16	9.97	0.8527	2.0586	0.5450		8.0893		17MS01.49	15	2	8.38	0.8546	1.0487	1.7677	1.4732
17MS01.17	70	7	9.93	0.8753	1.0525	2.1948		2.5031		17MS01.50	95	33	2.89	0.8817	1.0195	1.6856	1.9057
17MS01.18	46	12	3.89	0.9082	1.0402	2.0720		1.9266		17MS01.52	1	2	0.60	0.8931	1.1777	2.4336	1.4093
17MS01.20	1277	170	7.51	0.8974	0.9356	1.8199		2.3891		17MS01.53	663	253	2.62	0.8999	1.3397	2.9198	1.4218
17MS01.22	4	5	0.86	0.8559	1.0636	2.0625		1.1626		17MS01.56	45	15	3.13	0.8644	1.6027	2.6286	1.5413
17MS01.23	1316	1104	1.19	0.5093	2.3223	55.2046		1.8992		17MS01.57	462	467	0.99	0.8634	1.3099	4.1745	1.4078
17MS01.25	1583	70	22.75	0.8505	1.1378	2.6453		1.5710		17MS01.59	556	197	2.82	0.7957	3.2110	6.1032	2.3855
17MS01.27	122	19	6.25	0.8714	1.2965	1.7653		1.6522		17MS01.60	0	7	0.06	0.4696	3.8509	41.6457	2.0471
17MS01.28	118	19	6.24	0.8385	1.1699	1.6493		1.4157		17MS01.61	17	7	2.62	0.9328	1.2852	0.8348	2.5080
17MS01.31	2	1	1.86	0.9170	1.5418	0.7938		2.6302		17MS01.62	1801	509	3.54	0.9005	1.7886	2.2449	5.1810
17MS01.32	107	19	5.57	0.8156	1.2677	4.6167		1.3848		17MS01.63	851	210	4.05	0.4586	2.7958	56.5846	1.8309
17MS01.34	207	12	17.27	0.8531	1.3984	2.5556		1.3361

测点号	Th	U	Th/U	²⁰⁷Pb/²⁰⁶Pb			²⁰⁶Pb/²³⁸U			测点号	Th	U	Th/U	²⁰⁷Pb/²⁰⁶Pb		²⁰⁶Pb/²³⁸U
测点号	(10^-6)		Th/U	比值	1σ		比值		1σ	测点号	(10^-6)		Th/U	比值	1σ	比值	1σ
17MS01.2	1270	1181	1.08	0.5207	3.0654	49.087		1.8747		17MS01.35	464	472	0.98	0.8951	1.4044	1.3221	1.8974
17MS01.3	6878	249	27.66	0.891	1.2942	3.0512		4.23195		17MS01.37	123	25	4.93	0.5263	4.0704	39.6814	2.5101
17MS01.5	61	7	8.57	0.8688	1.2268	2.5613		1.1505		17MS01.38	1362	136	10.01	0.8535	1.3220	2.5465	4.5574
17MS01.6	1644	187	8.81	0.8868	1.3172	2.5214		1.7101		17MS01.39	56	16	3.37	0.8497	1.0897	2.7783	1.1734
17MS01.7	106	22	4.88	0.8586	1.2233	4.5204		1.2678		17MS01.40	5	17	0.28	0.8740	1.2181	1.0480	1.9597
17MS01.8	86	13	6.91	0.8760	1.1689	2.4897		1.3219		17MS01.42	196	30	6.50	0.8243	2.5830	0.6932	4.8606
17MS01.9	79	16	5.09	0.9095	1.1094	1.2497		2.1105		17MS01.43	59	7	8.42	0.9094	0.8948	0.1111	11.2151
17MS01.10	76	14	5.30	0.8834	1.5750	2.9378		1.5872		17MS01.44	192	52	3.69	0.5016	2.0304	44.7253	1.9601
17MS01.12	94	14	6.60	0.8743	1.4404	1.9390		1.5487		17MS01.45	1391	1995	0.70	0.6291	3.7503	30.8625	2.4905
17MS01.13	463	462	1.00	0.8804	1.3690	1.6412		1.3879		17MS01.46	1274	1874	0.68	0.5888	3.5811	35.6714	2.1179
17MS01.14	453	461	0.98	0.4845	3.3717	45.5478		2.3638		17MS01.47	6466	381	16.96	0.9039	1.4358	2.2080	3.0184
17MS01.16	155	16	9.97	0.8527	2.0586	0.5450		8.0893		17MS01.49	15	2	8.38	0.8546	1.0487	1.7677	1.4732
17MS01.17	70	7	9.93	0.8753	1.0525	2.1948		2.5031		17MS01.50	95	33	2.89	0.8817	1.0195	1.6856	1.9057
17MS01.18	46	12	3.89	0.9082	1.0402	2.0720		1.9266		17MS01.52	1	2	0.60	0.8931	1.1777	2.4336	1.4093
17MS01.20	1277	170	7.51	0.8974	0.9356	1.8199		2.3891		17MS01.53	663	253	2.62	0.8999	1.3397	2.9198	1.4218
17MS01.22	4	5	0.86	0.8559	1.0636	2.0625		1.1626		17MS01.56	45	15	3.13	0.8644	1.6027	2.6286	1.5413
17MS01.23	1316	1104	1.19	0.5093	2.3223	55.2046		1.8992		17MS01.57	462	467	0.99	0.8634	1.3099	4.1745	1.4078
17MS01.25	1583	70	22.75	0.8505	1.1378	2.6453		1.5710		17MS01.59	556	197	2.82	0.7957	3.2110	6.1032	2.3855
17MS01.27	122	19	6.25	0.8714	1.2965	1.7653		1.6522		17MS01.60	0	7	0.06	0.4696	3.8509	41.6457	2.0471
17MS01.28	118	19	6.24	0.8385	1.1699	1.6493		1.4157		17MS01.61	17	7	2.62	0.9328	1.2852	0.8348	2.5080
17MS01.31	2	1	1.86	0.9170	1.5418	0.7938		2.6302		17MS01.62	1801	509	3.54	0.9005	1.7886	2.2449	5.1810
17MS01.32	107	19	5.57	0.8156	1.2677	4.6167		1.3848		17MS01.63	851	210	4.05	0.4586	2.7958	56.5846	1.8309
17MS01.34	207	12	17.27	0.8531	1.3984	2.5556		1.3361

年代		区内构造活动	区内岩浆活动
古新世	晚期	胶莱盆地萎缩五莲—青岛—烟台断裂右旋挤压走滑
古新世	早期	胶莱盆地N—S向拉分五莲—青岛—烟台断裂右旋伸展走滑
晚白垩世	晚期	胶莱盆地NW—SE向伸展五莲—青岛—烟台断裂右旋伸展走滑	莒南火山角砾岩((66.8±1.5) Ma)^[50] 胶州玄武岩(72 Ma)^[51] 诸城玄武岩(76 Ma)^[51] 青岛基性脉岩((86.0±1.6) Ma)^[50]
晚白垩世	早期	胶莱盆地NW—SE向伸展五莲—青岛—烟台断裂右旋伸展走滑
早白垩世	中晚期	胶莱盆地早白垩世E—W向拉分五莲—青岛—烟台断裂E—W向伸展	分岭山安粗岩((110.4±1.7) Ma)^[52] 海阳安山质熔岩((118.06±3.22) Ma)^[29] 马山粗面英安岩((119.3±1.6) Ma)^[4] 七宝山次火山岩((126±3) Ma)^[46]
早白垩世	早期	胶莱盆地早白垩世E—W向拉分五莲—青岛—烟台断裂NW—SE向伸展
晚侏罗世	早期	胶莱盆地拉分五莲—青岛—烟台断裂左旋走滑	昆嵛山花岗闪长岩(147 Ma)^[46] 昆嵛山二长闪长岩((152.2±1.2) Ma)^[44] 鹊山二长花岗岩((154.0±1.2) Ma)^[44] 玲珑花岗闪长岩((153±4) Ma)^[42]
晚侏罗世	晚期	胶莱盆地拉分五莲—青岛—烟台断裂左旋走滑	鹊山石英二长岩((156.3±1.8) Ma)^[44] 文登二长花岗岩((157±5) Ma)^[43] 玲珑二长花岗岩((160±3) Ma)^[42] 玲珑金矿二长花岗岩((164±2) Ma)^[45]

年代		区内构造活动	区内岩浆活动
古新世	晚期	胶莱盆地萎缩五莲—青岛—烟台断裂右旋挤压走滑
古新世	早期	胶莱盆地N—S向拉分五莲—青岛—烟台断裂右旋伸展走滑
晚白垩世	晚期	胶莱盆地NW—SE向伸展五莲—青岛—烟台断裂右旋伸展走滑	莒南火山角砾岩((66.8±1.5) Ma)^[50] 胶州玄武岩(72 Ma)^[51] 诸城玄武岩(76 Ma)^[51] 青岛基性脉岩((86.0±1.6) Ma)^[50]
晚白垩世	早期	胶莱盆地NW—SE向伸展五莲—青岛—烟台断裂右旋伸展走滑
早白垩世	中晚期	胶莱盆地早白垩世E—W向拉分五莲—青岛—烟台断裂E—W向伸展	分岭山安粗岩((110.4±1.7) Ma)^[52] 海阳安山质熔岩((118.06±3.22) Ma)^[29] 马山粗面英安岩((119.3±1.6) Ma)^[4] 七宝山次火山岩((126±3) Ma)^[46]
早白垩世	早期	胶莱盆地早白垩世E—W向拉分五莲—青岛—烟台断裂NW—SE向伸展
晚侏罗世	早期	胶莱盆地拉分五莲—青岛—烟台断裂左旋走滑	昆嵛山花岗闪长岩(147 Ma)^[46] 昆嵛山二长闪长岩((152.2±1.2) Ma)^[44] 鹊山二长花岗岩((154.0±1.2) Ma)^[44] 玲珑花岗闪长岩((153±4) Ma)^[42]
晚侏罗世	晚期	胶莱盆地拉分五莲—青岛—烟台断裂左旋走滑	鹊山石英二长岩((156.3±1.8) Ma)^[44] 文登二长花岗岩((157±5) Ma)^[43] 玲珑二长花岗岩((160±3) Ma)^[42] 玲珑金矿二长花岗岩((164±2) Ma)^[45]

华北克拉通胶莱盆地马山地区粗面英安岩磷灰石U-Pb年代学及其地质意义

Apatite U-Pb Geochronology of the Trachy Dacite in Mashan Area, Jiaolai Basin, North China Craton, and Its Geological Significance

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