华北板块北缘东段三叠纪构造演化——来自辽北开原岩浆岩年代学、地球化学的证据

陈井胜; 李崴崴; 时溢; 李斌; 赵春强; 张立东

doi:10.18654/1000-0569/2022.08.03

华北板块北缘东段三叠纪构造演化——来自辽北开原岩浆岩年代学、地球化学的证据

陈井胜^1,2,,
李崴崴³,
时溢^1,2,
李斌^1,2,
赵春强^1,2,
张立东^1,2

- 1.
  中国地质调查局沈阳地质调查中心，沈阳 110034
- 2.
  东北地质科技创新中心，沈阳 110034
- 3.
  辽宁省地质矿产研究院有限责任公司，沈阳 110029
基金项目:
本文受国家自然科学基金项目(41902234、41872203)和中国地质调查局地调项目(DD20190042、DD20221632)联合资助

详细信息

作者简介:
陈井胜，1983年生，博士，教授级高级工程师，火成岩岩石学专业，E-mail: 5202268@qq.com

中图分类号: P588.124;P588.141;P597.3

收稿日期: 2022-03-01

修回日期: 2022-05-20

刊出日期: 2022-08-01

Evolution of the eastern segment of the northern margin of the North China Craton in the Triassic: Evidence from the geochronology and geochemistry of magmatic rocks in Kaiyuan area, North Liaoning

CHEN JingSheng^1,2,,
LI WeiWei³,
SHI Yi^1,2,
LI Bin^1,2,
ZHAO ChunQiang^1,2,
ZHANG LiDong^1,2

- 1.
  Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China
- 2.
  Northeast Geological S & T Innovation Center of China Geological Survey, Shenyang 110034, China
- 3.
  Liaoning Institute of Geology and Mineral Resources, Shenyang 110029, China

Received Date: 01 March 2022

Revised Date: 20 May 2022

Publish Date: 01 August 2022

摘要

摘要:
本文对华北板块北缘东段辽北开原地区辉长岩和流纹岩进行了岩相学、锆石U-Pb年代学和地球化学研究，结合前人资料探讨古亚洲洋东段三叠纪演化过程。锆石测年结果显示，辉长岩及流纹岩形成时代均为三叠纪(分别为246±2Ma、241±2Ma、226±3Ma及241±2Ma)。三期三叠纪辉长岩具有相似的地球化学特征，起源于地幔，并且在上升就位过程中均受到地壳物质的混染。其中，早三叠世辉长岩(246Ma)起源于受流体改造的富集型岩石圈地幔，由石榴石尖晶石二辉橄榄岩1%部分熔融形成，形成于俯冲板片断离导致的伸展环境；中三叠世辉长岩(241Ma)起源于受流体和熔体双重改造的过渡型岩石圈地幔，由石榴石尖晶石二辉橄榄岩1%~2%部分熔融形成；晚三叠世辉长岩(226Ma)起源于受流体和熔体双重改造的过渡型岩石圈地幔，由石榴石尖晶石二辉橄榄岩3%~4%部分熔融形成，形成于造山后的伸展拉张环境。中三叠世流纹岩(241Ma)富集轻稀土元素和大离子亲石元素，亏损高场强元素，亏损Nb、Ti、P、Sr元素等特征，属于后碰撞I型花岗岩，其低Sr低Yb特征暗示其源区深度为30~40km之间，其与中三叠世辉长岩构成“双峰式”火成岩，二者形成于岩石圈底部残余洋壳脱离导致的伸展环境。综合前人发表数据，根据年代学、岩石组合及地球化学特征可将华北板块北缘东段三叠纪岩浆活动划分为5期：252~246Ma、246~242Ma、242~240Ma、240~230Ma和230~215Ma。结合区域磨拉石建造、变质作用及蛇绿岩等资料，认为本区三叠纪经历了如下演化过程：(1)活动大陆边缘向同碰撞转换，古亚洲洋完成最终闭合(252~246Ma)；(2)持续挤压隆升造山(246~242Ma)；(3)南北挤压背景下，残余俯冲洋壳脱落导致的伸展(242~240Ma)；(4)持续挤压作用下快速隆升，地壳加厚(240~230Ma)；(5)造山后的伸展拉张环境(230~215Ma)。
- 华北板块北缘东段 /
- 三叠纪 /
- 辉长岩 /
- 锆石U-Pb年代学 /
- 构造演化
Abstract:
To constrain the evolution of the eastern segment of the Paleo-Asian Ocean (PAO), petrography, geochemistry and zircon U-Pb dating analyses were conducted over the gabbro and rhyolite in the Kaiyuan area, North Liaoning, in the eastern segment of the northern margin of the North China Craton (NCC). Zircon dating results indicate that the gabbros and rhyolite were formed in the Trassic (246±2Ma, 241±2Ma, 226±3Ma and 241±2Ma). The three gabbros of Triassic have similar geochemical characteristics, originated from the mantle, and were contaminated by crust materials in the process of ascending and emplacement. The Early Triassic gabbro (246Ma) originated from the enriched mantle source metasomatized by fluid. It was formed by 1% partial melting of garnet spinel lherzolite in the extensional environment caused by breaking off slab. The Middle Triassic gabbro (241Ma) was derived from a transitional mantle metasomatized by fluid and melt, and was formed by 1% to 2% partial melting of garnet spinel peridotite. The Late Triassic gabbro (226Ma) was derived from a transitional mantle metasomatized by fluid and melt, and was formed by 3%~4% partial melting of garnet spinel lherzolite in the post-orogenic extensional environment. The Middle Triassic rhyolite (241Ma) has the characteristic of post collisional I-type granite, that enriched in light rare earth elements and large ion lithophile elements, depleted in high field strength elements, and negative Nb, Ti, P and Sr anomaly. The low content of Sr and Yb suggested a 30~40km depth source. The Middle Trassic "bimodal" igneous rocks implied an extensional environment caused by the remainder oceanic crust breaked away at the bottom of the crust. Based on the lithologic association, regional strata information and the chronological data in this paper and published by predecessors, the Triassic magmatism in the eastern segment of the northern margin of the NCC can be divided into five stages: 252~246Ma, 246~242Ma, 242~240Ma, 240~230Ma and 230~215Ma. These five magmatic events were the results of the southward subduction and extinction of the PAO: (1) The transformation from active continental margin to syn-collisional setting resulted in the final closure of the PAO (252~246 Ma); (2) Continuous pushing resulted in orogenic uplift (246~242Ma); (3) Extension caused by the detachment of the remainder subduction oceanic crust at the bottom of the crust (242~240Ma); (4) Rapid uplift and crustal thickening (240~230Ma); (5) Extension of post-orogenic(230~215Ma).
- The eastern segment of the northern margin of the NCC /
- Trassic /
- Gabbro /
- Zircon U-Pb chronology /
- Tectonic evolution

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图 1

研究区构造位置(a，据 Li, 2006修改)和华北板块北缘东段三叠纪岩浆岩分布图(b)

Figure 1.

The tectonic location (a, modified after Li, 2006) and distribution of Triassic magmatic rocks (b) of study area

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图 2

研究区地质简图

Figure 2.

Simplified geological map of the study area

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图 3

辽北开原地区岩浆岩样品的野外及其显微照片

Figure 3.

Occurrence and micro-pictures of magmatic rocks from the Kaiyuan area, North Liaonin

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图 4

开原地区岩浆岩部分锆石阴极发光图像

Figure 4.

CL images of the selected zircons of magmatic rocks from the Kaiyuan area

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图 5

开原地区岩浆岩锆石U-Pb年龄谐和图

Figure 5.

Zircons U-Pb ages of magmatic rocks from the Kaiyuan area

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图 6

开原地区岩浆岩SiO₂-(Na₂O+K₂O)图解(a, 据 Middlemost，1994)、R1-R2图解(b, 据 Roche et al., 1980)、SiO₂-K₂O图解(c, 据 Peccerillo and Taylor, 1976)和A/NK-A/CNK图解(d, 据 Maniar and Piccoli, 1989)

Figure 6.

Diagrams of SiO₂ vs. total alkali (Na₂O+K₂O) (a, after Middlemost, 1994), R1 vs. R2(b, after Roche et al., 1980), SiO₂-K₂O (c, after Peccerillo and Taylor, 1976) and A/NK vs. A/CNK (d, after Maniar and Piccoli, 1989) for magmatic rocks from the Kaiyuan area

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图 7

开原地区岩浆岩球粒陨石标准化稀土元素配分图(a、c)和原始地幔标准化微量元素蛛网图(b、d)

Figure 7.

Chondrite-normalized rare earth element patterns (a, c) and primitive mantle-normalized trace element spider diagrams (b, d) for these magmatic rocks from the Kaiyuan area

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图 8

华北板块北缘东段三叠纪岩浆岩年龄频谱图

Figure 8.

Age histogram of magmatic rocks from the eastern segment of the northern margin of NCC

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图 9

开原地区辉长岩Zr与主、微量元素相关图

Figure 9.

Zr against selected major and trace elements' variation diagrams for gabbro from the Kaiyuan area

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图 10

开原地区三叠纪辉长岩源区判别图解

Figure 10.

Source characteristics of the Triassic gabbros from the Kaiyuan area

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图 11

开原地区中三叠世流纹岩成因判别图解(底图据 Whalen et al., 1987)

Figure 11.

Genesis diagram of the Middle Triassic rhyolite from the Kaiyuan area (base map after Whalen et al., 1987)

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图 12

开原地区三叠纪岩浆岩构造环境判别图解

Figure 12.

Identification diagrams of tectonic setting for the Triassic magmatic rocks from the Kaiyuan area

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图 13

华北板块北缘法库-长春-延吉三叠纪构造演化模型

Figure 13.

A cartoon model for the Trissic tectonic evolution of the northern margin of the NCC from Faku, Changchun to Yanji

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表 1

辽北开原地区岩浆岩同位素样品采集点及岩性

Table 1.

Location and lithology for the magmatic rocks from the Kaiyuan area, North Liaoning

样品号	位置	岩性	测年结果(Ma)
D2009	124°34′24.92″E、42°27′48.32″N	细粒辉长岩	246±2
D2007	124°25′49.91″E、42°31′51.69″N	变质中细粒辉长岩	241±2
D2011	124°17′59.51″E、42°22′35.68″N	辉长岩	226±3
D2034	124°22′35.34″E、42°32′01.43″N	变流纹岩	241±2

下载: 导出CSV

表 2

开原三叠纪岩浆岩样品中锆石LA-ICP-MS U-Pb分析结果

Table 2.

LA-ICP-MS zircon U-Pb dating data of Trassic magmatic rocks from the Kaiyuan area

测点号	Th	U	Pb	Th/U	同位素比值						年龄(Ma)
	(×10^-6)				²⁰⁷Pb/²³⁵U			²⁰⁶Pb/²³⁸U			²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U
	(×10^-6)				比值	1σ		比值	1σ		比值	1σ	比值	1σ
D2009细粒辉长岩
-1	186	466	21	0.40	0.27372	0.01277		0.03830	0.00096		246	10	242	6
-2	4010	2254	137	1.78	0.27466	0.00955		0.03833	0.00092		246	8	242	6
-3	289	520	44	0.56	0.27421	0.01065		0.03849	0.00094		246	8	243	6
-4	295	689	30	0.43	0.27864	0.01127		0.03897	0.00095		250	9	246	6
-5	386	755	30	0.51	0.27399	0.01291		0.03827	0.00096		246	10	242	6
-6	2179	1755	95	1.24	0.27762	0.00897		0.03865	0.00092		249	7	244	6
-7	4810	4369	233	1.10	0.27764	0.00762		0.03898	0.00092		249	6	247	6
-8	572	1204	55	0.47	0.27592	0.00921		0.03925	0.00094		247	7	248	6
-9	186	386	57	0.48	0.28079	0.01253		0.03907	0.00098		251	10	247	6
-10	773	872	42	0.89	0.27376	0.01008		0.03848	0.00094		246	8	243	6
-11	2303	2156	108	1.07	0.26937	0.00847		0.03818	0.00092		242	7	242	6
-12	922	1485	71	0.62	0.27820	0.00896		0.03966	0.00096		249	7	251	6
-13	364	591	46	0.62	0.26351	0.01068		0.03886	0.00097		237	9	246	6
-14	1102	1317	52	0.84	0.27648	0.00932		0.03900	0.00096		248	7	247	6
-15	2153	2142	110	1.01	0.28204	0.00855		0.03971	0.00096		252	7	251	6
-16	300	636	28	0.47	0.28446	0.01563		0.03945	0.00105		254	12	249	7
-17	833	1168	54	0.71	0.28147	0.00990		0.03931	0.00097		252	8	249	6
-18	273	416	19	0.66	0.27293	0.01507		0.03932	0.00104		245	12	249	6
-19	1742	2571	119	0.68	0.28226	0.01114		0.03954	0.00101		252	9	250	6
D2007变质中细粒辉长岩
-1	65	92	5	0.71	0.28905	0.02397		0.03880	0.00111		258	19	245	7
-2	73	84	4	0.87	0.27952	0.01389		0.03868	0.00105		250	11	245	7
-3	77	103	5	0.74	0.26258	0.01262		0.03925	0.00105		237	10	248	7
-4	49	67	3	0.73	0.29372	0.03029		0.03845	0.00107		261	24	243	7
-5	42	61	3	0.69	0.28433	0.01686		0.03889	0.00107		254	13	246	7
-6	80	101	5	0.79	0.27880	0.01381		0.03867	0.00102		250	11	245	6
-7	73	89	5	0.82	0.26990	0.01554		0.03818	0.00103		243	12	242	6
-8	101	151	8	0.67	0.29417	0.01950		0.03842	0.00099		262	15	243	6
-9	36	54	3	0.66	0.27078	0.02675		0.03857	0.00128		243	21	244	8
-10	41	69	3	0.59	0.28528	0.03548		0.03823	0.00119		255	28	242	7
-11	79	112	6	0.71	0.27183	0.01299		0.03855	0.00108		244	10	244	7
-12	66	92	5	0.72	0.26398	0.01381		0.03760	0.00097		238	11	238	6
-13	72	86	4	0.83	0.29873	0.02042		0.03560	0.00096		265	16	226	6
-14	114	120	6	0.95	0.27431	0.01425		0.03789	0.00098		246	11	240	6
-15	129	119	7	1.09	0.27206	0.01562		0.03823	0.00100		244	12	242	6
-16	105	141	7	0.75	0.27825	0.01258		0.03803	0.00095		249	10	241	6
-17	67	95	5	0.71	0.26340	0.01711		0.03732	0.00101		237	14	236	6
-18	81	108	6	0.74	0.26990	0.01415		0.03802	0.00098		243	11	241	6
-19	82	119	6	0.69	0.28183	0.01743		0.03801	0.00095		252	14	240	6
-20	135	138	8	0.98	0.27606	0.01381		0.03801	0.00096		248	11	240	6
-21	65	97	5	0.67	0.26871	0.01547		0.03723	0.00097		242	12	236	6
-22	67	78	4	0.86	0.26827	0.02629		0.03753	0.00101		241	21	238	6
-23	141	178	9	0.79	0.27931	0.01258		0.03750	0.00091		250	10	237	6
D2011辉长岩
-1	133	131	40	1.02	0.25322	0.06683		0.03569	0.00225		229	54	226	14
-2	123	143	30	0.86	0.25584	0.03335		0.03571	0.00130		231	27	226	8
-3	132	87	16	1.52	0.25477	0.07895		0.03598	0.00260		230	64	228	16
-4	315	207	34	1.52	0.24825	0.02498		0.03552	0.00116		225	20	225	7
-5	245	144	22	1.70	0.24573	0.02975		0.03581	0.00129		223	24	227	8
-6	140	148	18	0.95	0.24190	0.04657		0.03453	0.00168		220	38	219	10
-7	531	260	34	2.04	0.24320	0.01631		0.03524	0.00098		221	13	223	6
-8	101	115	11	0.88	0.23129	0.04962		0.03419	0.00177		211	41	217	11
-9	156	130	11	1.19	0.25270	0.04906		0.03573	0.00179		229	40	226	11
-10	119	125	9	0.96	0.24980	0.04319		0.03682	0.00166		226	35	233	10
-11	70	109	7	0.64	0.24551	0.03742		0.03548	0.00145		223	31	225	9
-12	54	68	5	0.79	0.25392	0.03853		0.03541	0.00142		230	31	224	9
-13	42	68	4	0.61	0.24755	0.03375		0.03572	0.00137		225	27	226	9
-14	163	166	11	0.98	0.24227	0.02035		0.03631	0.00109		220	17	230	7
-15	52	97	5	0.54	0.24680	0.02787		0.03508	0.00119		224	23	222	7
-16	69	141	8	0.49	0.24069	0.03240		0.03508	0.00136		219	27	222	8
-17	78	104	6	0.74	0.25224	0.05729		0.03661	0.00205		228	46	232	13
-18	41	52	3	0.79	0.24152	0.04105		0.03454	0.00146		220	34	219	9
-19	91	140	7	0.65	0.25280	0.03260		0.03587	0.00135		229	26	227	8
-20	38	57	3	0.66	0.25690	0.08253	0.03580	0.00263	232	67	227	16
-21	50	74	3	0.68	0.25510	0.03262	0.03631	0.00131	231	26	230	8
-22	30	57	3	0.52	0.25208	0.03631	0.03626	0.00139	228	29	230	9
-23	40	73	3	0.54	0.25647	0.03027	0.03643	0.00131	232	24	231	8
-24	58	104	5	0.56	0.25760	0.05780	0.03719	0.00208	233	47	235	13
D2034变流纹岩
-1	432	923	36	0.47	0.27334	0.01467	0.03864	0.00102	245	12	244	6
-2	297	423	20	0.70	0.27585	0.02298	0.03879	0.00118	247	18	245	7
-3	347	447	21	0.78	0.27122	0.01273	0.03820	0.00098	244	10	242	6
-4	199	234	11	0.85	0.25779	0.02716	0.03716	0.00125	233	22	235	8
-5	171	228	11	0.75	0.26933	0.01680	0.03815	0.00104	242	13	241	6
-6	263	343	16	0.77	0.25793	0.01970	0.03752	0.00109	233	16	237	7
-7	239	287	13	0.83	0.26931	0.01976	0.03748	0.00108	242	16	237	7
-8	349	737	33	0.47	0.26794	0.01312	0.03885	0.00100	241	11	246	6
-9	104	98	5	1.05	0.26130	0.03957	0.03786	0.00154	236	32	240	10
-10	497	719	34	0.69	0.27876	0.01819	0.03878	0.00108	250	14	245	7
-11	289	691	30	0.42	0.26904	0.01103	0.03849	0.00096	242	9	243	6
-12	356	647	29	0.55	0.27136	0.01149	0.03851	0.00097	244	9	244	6
-13	143	208	9	0.69	0.26947	0.02728	0.03895	0.00127	242	22	246	8
-14	313	378	18	0.83	0.26661	0.02122	0.03793	0.00112	240	17	240	7
-15	298	433	20	0.69	0.26736	0.01346	0.03864	0.00099	241	11	244	6
-16	541	713	72	0.76	0.27282	0.00980	0.03764	0.00093	245	8	238	6
-17	218	300	14	0.73	0.27191	0.02253	0.03800	0.00114	244	18	240	7
-18	161	234	11	0.69	0.26743	0.02336	0.03755	0.00115	241	19	238	7
-19	238	182	9	1.31	0.26853	0.04507	0.03741	0.00165	242	36	237	10
-20	350	588	90	0.60	0.27082	0.01259	0.03861	0.00098	243	10	244	6
-21	157	380	17	0.41	0.27230	0.01729	0.03841	0.00105	245	14	243	7
-22	253	640	28	0.40	0.26807	0.01208	0.03860	0.00098	241	10	244	6
-23	774	1715	74	0.45	0.26807	0.01623	0.03783	0.00102	241	13	239	6
-24	226	350	16	0.65	0.26863	0.07344	0.03894	0.00248	242	59	246	15

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表 3

开原三叠纪岩浆岩主量元素(wt%)、稀土元素和微量元素(×10^-6)分析结果

Table 3.

Major (wt%) and trace element (×10^-6) compositions of Trassic magmatic rocks from the Kaiyuan area

样品号		D2009-Q1	-Q2	-Q3	-Q4	-Q5	-Q6	-Q7		D2007-Q1	-Q2	-Q3	-Q4	-Q5	-Q6
岩性		早三叠世细粒辉长岩								中三叠世变质中细粒辉长岩
SiO₂		50.00	50.19	49.84	49.51	49.73	50.10	50.10		48.82	50.13	45.49	49.99	47.93	50.40
TiO₂		0.99	0.96	1.06	1.07	0.98	1.07	1.14		2.10	2.12	2.16	2.10	2.15	2.10
Al₂O₃		19.19	19.35	19.65	18.51	19.59	19.49	19.33		14.72	14.26	14.79	14.40	14.68	14.52
Fe₂O₃		3.53	3.17	2.09	3.87	4.02	1.67	1.96		3.54	2.34	5.56	2.31	4.03	2.81
FeO		6.51	6.34	6.69	6.74	6.26	6.95	7.95		9.06	9.45	8.97	9.66	9.16	9.01
MnO		0.12	0.11	0.15	0.12	0.12	0.15	0.15		0.19	0.18	0.16	0.16	0.15	0.15
MgO		4.09	4.89	4.20	3.83	4.15	4.42	3.60		6.06	6.25	6.18	6.04	6.00	5.75
CaO		6.33	5.91	6.59	5.92	6.20	6.66	6.66		7.21	6.97	7.30	6.87	7.19	6.61
Na₂O		4.75	4.98	5.22	5.45	4.69	4.89	5.18		3.23	3.31	3.15	3.27	3.37	3.38
K₂O		2.13	2.06	2.12	2.37	2.12	2.23	2.18		1.64	1.53	1.85	1.75	1.65	1.76
P₂O₅		0.36	0.34	0.39	0.32	0.37	0.36	0.36		0.38	0.35	0.42	0.37	0.40	0.38
LOI		1.99	1.70	2.04	2.29	1.80	1.90	1.62		2.98	3.00	3.34	2.89	3.20	3.03
Total		99.99	100.0	100.0	99.99	100.0	99.90	100.2		99.91	99.91	99.37	99.82	99.90	99.91
Mg^#		32.6	37.3	32.6	30.4	33.8	32.9	25.9		34.0	33.8	34.7	32.6	33.6	33.0
A/NK		1.9	1.86	1.81	1.61	1.96	1.86	1.78		2.08	2	2.06	1.98	2.01	1.94
A/CNK		0.92	0.95	0.9	0.87	1.02	0.9	0.87		0.76	0.75	0.76	0.76	0.76	0.78
R1		1055	1007	910	700	1041	1030	1015		1629	1745	1360	1703	1507	1672
R2		1282	1276	1326	1211	1269	1341	1288		1403	1378	1436	1360	1401	1319
La		40.4	55.2	35.2	30.7	49.6	36.5	28.8		22.9	19.9	22.2	21.7	21.2	23.3
Ce		78.1	99.2	70.2	61.9	92.3	68.8	59.4		43.3	38.8	43.1	41.3	41.1	43.7
Pr		10.0	12.2	9.87	8.57	11.6	9.22	8.52		6.06	5.45	6.05	5.78	5.70	6.19
Nd		36.6	40.3	35.8	32.5	41.3	35.6	33.5		26.6	24.1	26.3	25.1	24.9	27.2
Sm		7.59	7.31	6.42	6.08	6.91	6.94	7.00		5.57	5.15	5.77	5.27	5.23	5.61
Eu		1.89	1.85	2.23	2.12	2.08	1.92	1.87		2.31	2.11	2.38	2.15	2.24	2.28
Gd		5.26	5.41	6.04	5.72	5.24	5.44	5.07		5.13	4.71	5.04	4.82	4.75	5.08
Tb		0.70	0.69	0.84	0.81	0.76	0.79	0.71		0.88	0.82	0.91	0.84	0.84	0.89
Dy		3.77	3.51	4.22	3.66	3.49	3.74	3.64		4.62	4.40	4.82	4.55	4.34	4.64
Ho		0.69	0.65	0.86	0.73	0.66	0.73	0.81		0.88	0.86	0.90	0.86	0.82	0.89
Er		2.07	2.12	2.30	2.20	1.87	1.98	2.18		2.28	2.23	2.34	2.27	2.15	2.28
Tm		0.36	0.29	0.37	0.32	0.29	0.20	0.38		0.35	0.33	0.34	0.34	0.33	0.34
Yb		2.25	1.79	2.13	1.83	1.96	1.61	2.06		2.24	2.09	2.19	2.15	2.01	2.19
Lu		0.30	0.33	0.34	0.32	0.34	0.28	0.30		0.31	0.30	0.32	0.31	0.29	0.31
ΣREE		190.0	230.8	176.7	157.5	218.4	173.7	154.3		123.5	111.3	122.7	117.4	115.9	124.9
LREE		174.6	216.0	159.7	141.9	203.7	158.9	139.1		106.8	95.51	105.8	101.3	100.4	108.2
HREE		15.40	14.79	17.09	15.59	14.63	14.77	15.14		16.68	15.75	16.85	16.13	15.53	16.62
LREE/HREE		11.34	14.61	9.34	9.10	13.93	10.76	9.19		6.40	6.06	6.28	6.28	6.46	6.51
(La/Yb)_N		12.85	22.15	11.86	12.04	18.12	16.23	10.02		7.36	6.82	7.28	7.25	7.55	7.63
δEu		0.92	0.90	1.10	1.10	1.06	0.95	0.96		1.32	1.31	1.35	1.30	1.37	1.31
δCe		0.95	0.94	0.92	0.94	0.94	0.92	0.93		0.90	0.91	0.91	0.90	0.92	0.89
Y		18.8	17.7	21.8	20.6	18.5	19.6	20.0		22.2	20.7	22.5	21.4	21.2	22.2
V		116	108	127	134	111	127	148		293	297	310	303	299	294
Cr		16.0	7.44	10.2	13.6	8.05	8.76	10.1		98.6	98.5	107	167	105	101
Co		16.5	15.3	20.2	21.1	16.3	20.0	23.9		68.5	60.0	61.6	56.7	66.9	62.7
Ni		6.36	2.49	2.58	7.46	2.28	4.02	7.08		82.3	75.2	66.7	72.4	69.7	77.6
Be		1.66	1.62	1.58	1.46	1.61	1.63	1.59		0.95	0.98	0.94	1.03	0.94	0.97
Rb		52.6	51.5	44.4	45.3	52.6	40.7	46.2		38.0	35.9	40.1	40.4	38.1	42.5
Sr		863	862	870	743	861	839	902		439	429	372	406	412	423
Ba		699	753	671	995	671	740	710		715	737	682	839	650	733
Zr		194	261	221	191	216	180	183		117	101	111	111	100	117
Nb		8.00	8.20	8.97	8.26	8.55	6.72	7.48		8.96	8.96	9.15	8.59	10.7	10.2
Hf		5.54	6.88	6.02	4.78	6.38	5.19	5.68		3.65	3.36	3.61	3.57	3.11	3.64
Ta		0.55	0.55	0.65	0.48	0.80	0.40	0.63		0.63	0.62	0.60	0.61	0.64	0.67
Th		2.69	2.59	2.74	3.64	3.05	2.29	1.99		2.45	2.04	2.13	1.65	1.67	2.05
U		0.79	0.78	0.80	0.52	0.87	0.44	0.50		0.37	0.42	0.42	0.29	0.32	0.34
Ga		21.7	21.4	23.5	20.3	22.3	22.1	22.7		24.3	28.5	28.7	22.8	21.9	23.4
(La/Sm)_N		3.44	4.88	3.54	3.26	4.64	3.39	2.66		2.66	2.50	2.48	2.66	2.62	2.68
La/Sm		5.32	7.55	5.48	5.04	7.18	5.26	4.12		4.12	3.87	3.85	4.12	4.06	4.15
Ta/Yb		0.25	0.31	0.31	0.26	0.41	0.25	0.31		0.28	0.29	0.27	0.28	0.32	0.30
Th/Yb		1.19	1.45	1.29	1.99	1.55	1.42	0.96		1.10	0.97	0.97	0.77	0.83	0.94
La/Yb		17.92	30.88	16.54	16.78	25.26	22.63	13.97		10.26	9.51	10.15	10.11	10.53	10.64
Zr/Y		10.28	14.74	10.11	9.26	11.69	9.17	9.18		5.26	4.90	4.95	5.20	4.72	5.26
Nb/Th		2.97	3.17	3.28	2.27	2.80	2.93	3.76		3.66	4.40	4.30	5.22	6.41	4.96
Ba/Nb		87.35	91.84	74.80	120.5	78.51	110.2	94.97		79.79	82.32	74.53	97.64	60.84	71.93
Th/Yb		1.19	1.45	1.29	1.99	1.55	1.42	0.96		1.10	0.97	0.97	0.77	0.83	0.94
Zr/Nb	24.18	31.84	24.60	23.14	25.30	26.80	24.52	13.01	11.31	12.16	12.93	9.39	11.45
Ba/La	17.31	13.64	19.10	32.46	13.53	20.28	24.65	31.18	37.04	30.73	38.69	30.66	31.50
La/Nb	5.05	6.73	3.92	3.71	5.80	5.43	3.85	2.56	2.22	2.43	2.52	1.98	2.28
Nb/La	0.20	0.15	0.26	0.27	0.17	0.18	0.26	0.32	0.29	0.27	0.22	0.28	0.28
Hf/Ta	10.00	12.44	9.20	10.04	7.96	12.99	9.00	5.68	8.68	10.88	19.51	7.23	7.21
La/Ta	72.86	99.70	53.75	64.35	61.89	91.37	45.65	23.34	34.28	43.74	86.23	27.81	29.09
Th/Ta	4.85	4.67	4.19	7.64	3.80	5.73	3.15	14.14	20.79	30.21	51.02	19.22	21.71

样品号		D2034-Q1	-Q2	-Q3	-Q4	-Q6	-Q7			D2011-Q1	-Q2	-Q3	-Q4	-Q5	-Q6	-Q7
岩性		中三叠世变流纹岩								晚三叠世辉长岩
SiO₂		65.84	65.83	66.52	65.98	65.67	67.90			52.10	50.86	51.98	51.56	49.93	50.12	49.02
TiO₂		0.46	0.45	0.47	0.45	0.46	0.44			1.63	1.68	1.55	1.54	1.66	1.68	1.59
Al₂O₃		15.93	15.79	15.93	16.30	15.86	16.01			16.35	16.70	16.10	16.43	16.54	16.19	16.81
Fe₂O₃		3.02	2.93	2.91	3.72	3.22	2.28			1.48	1.53	1.50	1.60	2.21	1.91	2.53
FeO		0.87	0.80	1.06	0.52	0.71	1.01			7.09	6.90	6.50	6.72	6.77	7.01	7.06
MnO		0.07	0.07	0.08	0.06	0.07	0.05			0.13	0.14	0.13	0.14	0.14	0.15	0.15
MgO		0.93	1.14	0.74	0.42	1.14	0.61			6.30	5.74	6.23	6.49	6.23	6.29	7.19
CaO		1.86	1.93	2.32	1.63	1.91	1.35			7.19	6.70	6.87	7.27	7.60	7.55	8.32
Na₂O		3.15	3.49	3.58	3.17	3.16	3.29			4.07	4.05	4.03	3.68	3.78	3.70	3.30
K₂O		6.25	5.94	5.07	6.21	6.20	5.46			1.36	2.09	1.60	1.50	1.65	1.56	1.47
P₂O₅		0.083	0.081	0.092	0.086	0.088	0.079			0.29	0.31	0.29	0.30	0.31	0.32	0.33
LOI		1.37	1.38	1.06	1.29	1.32		1.39		2.32	3.33	3.27	2.79	3.17	3.20	2.22
Total		99.82	99.81	99.83	99.84	99.80	99.86			100.3	100.0	100.0	100.0	99.99	99.67	99.99
Mg^#		45.3	52.3	35.1	38.6	55.3		31.6		40.7	39.1	42.5	42.7	41.5	40.9	44.0
A/NK		1.33	1.3	1.4	1.37	1.33	1.41			2	1.87	1.93	2.14	2.07	2.08	2.39
A/CNK		1.05	1.02	1.04	1.11	1.05	1.18			0.8	0.82	0.8	0.81	0.78	0.78	0.79
R1		1780	1732	1943	1787	1774	2063			1663	1428	1635	1745	1551	1628	1683
R2		567	583	605	524	581	497			1432	1374	1405	1462	1494	1490	1612
La		41.3	41.1	42.7	46.0	42.2	42.1			17.7	18.0	15.9	18.1	19.6	17.8	17.2
Ce		78.9	78.0	81.0	85.3	79.8	80.9			39.2	38.2	36.5	39.4	42.7	37.9	39.6
Pr		9.15	8.89	9.09	9.88	9.20	9.15			5.95	5.68	5.46	5.59	6.04	5.46	6.17
Nd		31.9	31.6	32.3	33.6	32.8	32.1			24.1	24.6	24.3	24.0	25.1	21.3	25.1
Sm		5.13	5.11	5.18	5.55	5.20	5.18			5.75	5.63	5.31	5.63	5.95	4.73	6.35
Eu		1.28	1.36	1.32	1.42	1.34	1.31			1.76	1.80	1.82	1.72	1.92	1.48	2.04
Gd		4.80	4.67	4.87	4.93	4.88	4.94			5.25	5.10	5.28	5.29	4.89	4.53	5.57
Tb		0.63	0.62	0.65	0.67	0.66	0.64			0.76	0.78	0.72	0.85	0.87	0.65	0.90
Dy		3.11	2.99	2.98	3.00	3.07	2.99			4.29	4.49	4.32	4.13	4.62	3.64	4.10
Ho		0.56	0.53	0.54	0.55	0.58	0.54			0.81	0.89	0.78	0.92	0.97	0.75	0.86
Er		1.56	1.40	1.49	1.49	1.60	1.48			2.35	2.58	2.21	2.48	2.52	2.24	2.47
Tm		0.25	0.25	0.25	0.24	0.28	0.25			0.30	0.33	0.29	0.30	0.43	0.34	0.34
Yb		1.73	1.63	1.64	1.62	1.65	1.59			2.00	2.19	1.97	2.16	2.13	1.86	2.13
Lu		0.28	0.24	0.26	0.26	0.26	0.26			0.30	0.33	0.33	0.30	0.34	0.31	0.38
ΣREE		180.6	178.3	184.2	194.4	183.5	183.5			110.6	110.6	105.2	110.8	118.1	103.0	113.1
LREE		167.6	166.0	171.5	181.7	170.6	170.8			94.53	93.94	89.27	94.39	101.3	88.66	96.38
HREE		12.93	12.33	12.69	12.75	12.96	12.68			16.06	16.69	15.91	16.43	16.77	14.32	16.74
LREE/HREE		12.97	13.46	13.51	14.24	13.16	13.46			5.89	5.63	5.61	5.74	6.04	6.19	5.76
(La/Yb)_N		17.08	18.14	18.63	20.38	18.40	19.05			6.35	5.91	5.79	6.00	6.60	6.86	5.78
δEu		0.79	0.85	0.80	0.83	0.81	0.79			0.98	1.02	1.05	0.97	1.09	0.97	1.05
δCe		1.00	1.00	1.01	0.98	0.99	1.01			0.94	0.93	0.96	0.96	0.96	0.94	0.94
Y		15.2	14.4	15.1	15.0	15.5	15.0			21.9	21.3	21.7	23.3	22.6	18.1	22.1
V		24.1	24.9	26.6	25.9	28.0	26.4			187	185	187	178	197	197	190
Cr		10.1	13.5	12.5	9.91	11.5	10.8			129	97.1	243	133	132	111	129
Co		5.52	5.33	6.14	4.90	5.35	4.71			35.9	32.1	34.3	34.0	32.6	36.8	36.3
Ni		10.7	11.7	13.1	10.2	13.6	10.2			62.9	53.9	70.7	64.3	63.5	63.0	66.7
Be		2.45	2.60	3.14	2.54	2.53	2.55			1.22	1.29	1.70	1.13	1.33	1.04	1.16
Rb		132	132	121	139	143	141			29.8	45.7	36.9	32.3	35.4	32.8	28.8
Sr		147	253	254	149	208	148			674	652	647	652	635	653	660
Ba		404	425	415	498	426	461			433	501	340	387	346	334	469
Zr		254	260	261	261	262	255			104	112	105	112	121	93.5	116
Nb		13.4	11.7	11.6	10.1	11.8	11.9			5.53	6.60	5.43	6.03	6.54	5.94	5.36
Hf		10.0	10.4	10.6	10.4	11.0	10.4			3.61	3.15	3.20	3.13	4.21	2.87	4.00
Ta		1.77	1.20	0.98	0.53	1.52	1.45			0.34	0.48	0.32	0.36	0.37	0.34	0.36
Th		25.0	24.9	29.5	27.2	29.2	31.4			1.43	1.05	0.94	1.10	1.33	1.17	1.05
U		4.29	4.19	4.69	4.41	5.10	4.54			0.35	0.31	0.33	0.34	0.35	0.35	0.44
Ga		19.7	18.6	18.9	20.7	20.6	20.4			19.4	17.7	18.8	18.1	18.0	19.2	18.3
(La/Sm)_N		5.20	5.19	5.31	5.34	5.24	5.25			1.99	2.07	1.93	2.07	2.13	2.42	1.75
La/Sm		8.05	8.04	8.23	8.28	8.11	8.13			3.07	3.20	2.99	3.21	3.30	3.75	2.71
Ta/Yb		1.02	0.74	0.59	0.33	0.92	0.91			0.17	0.22	0.16	0.17	0.17	0.18	0.17
Th/Yb		14.43	15.34	17.94	16.81	17.73	19.82			0.71	0.48	0.48	0.51	0.63	0.63	0.49
La/Yb		23.81	25.29	25.97	28.41	25.65	26.56			8.85	8.24	8.07	8.36	9.20	9.56	8.06
Zr/Y		16.70	18.05	17.36	17.35	16.90	17.01			4.75	5.28	4.84	4.80	5.35	5.18	5.27
Nb/Th		0.54	0.47	0.39	0.37	0.40	0.38			3.87	6.29	5.76	5.49	4.90	5.07	5.13
Ba/Nb		30.20	36.19	35.82	49.05	36.23	38.81			78.31	75.81	62.57	64.21	52.91	56.19	87.57
Th/Yb		14.43	15.34	17.94	16.81	17.73	19.82			0.71	0.48	0.48	0.51	0.63	0.63	0.49
Zr/Nb	19.01	22.10	22.54	25.70	22.33	21.48		18.84	16.99	19.30	18.51	18.51	15.74	21.71
Ba/La	9.79	10.34	9.73	10.82	10.08	10.94		24.48	27.80	21.35	21.40	17.64	18.79	27.33
La/Nb	3.08	3.50	3.68	4.53	3.59	3.55		3.20	2.73	2.93	3.00	3.00	2.99	3.20
Nb/La	0.39	0.45	0.41	0.40	0.50	0.44		0.31	0.37	0.34	0.33	0.33	0.33	0.31
Hf/Ta	5.80	5.46	6.02	5.85	4.83	5.46		10.50	6.58	10.12	8.63	11.45	8.53	11.17
La/Ta	36.47	32.33	37.02	35.60	32.90	34.92		51.45	37.59	50.30	49.78	53.32	52.76	48.01
Th/Ta	3.90	3.31	3.55	2.70	2.59	3.08		4.16	2.19	2.98	3.02	3.63	3.48	2.92

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表 4

华北板块北缘东段三叠纪岩浆岩地质年代学数据汇总

Table 4.

Summary of geochronological data for Triassic igneous rocks in the eastern segment of the northern margin of NCC

序号	样品号	采样位置	侵入体	岩性	测试方法(锆石U-Pb)	年龄(Ma)	参考文献
252~246Ma
1	JHS3-1	E127°09′45″、N43°00′55″	色洛河	高镁安山岩	SHRIMP	252±5	李承东等，2007
2	FX06-52	E121°38′38″、N42°17′36″		镁铁质岩	LA-ICP-MS	252±2	Zhang et al., 2010
3	DY143-2	E125°51′48″、N43°02′31″	安怡	二长花岗岩	LA-ICP-MS	252±2	Wu et al., 2011
4		E130°00′46″、N43°07′37″		花岗闪长岩	LA-ICP-MS	252±1	付长亮等，2010
5	JK13-1	E127°41′31″、N42°58′59″	黄泥岭	二长花岗岩	LA-ICP-MS	252±1	王子进，2016
6	13JH3-1	E127°20′48″、N43°59′42″	秃顶	角闪辉长岩	LA-ICP-MS	252±1	王子进，2016
7	13JH1-1	E125°59′52″、N43°26′42″	山河	石英二长闪长岩	LA-ICP-MS	252±1	王子进，2016
8	RZ08	E124°40′40″、N42°25′10″	尖山子	二长花岗岩	LA-ICP-MS	251±2	刘锦等，2016
9	YZ02-49	E129°30′00″、N42°39′39″	龙阳洞	石英闪长岩	LA-ICP-MS	251±2	Wu et al., 2011
10	DY123-4	E125°57′29″、N43°06′40″	大红石砬子	碱长花岗岩	LA-ICP-MS	251±2	Wu et al., 2011
11	18FK020-1	法库东南	前榆村	辉长闪长岩	LA-ICP-MS	252±2	Jing et al., 2022
12	CK30	E123°34′05″、N42°10′56″		弱变形花岗岩	LA-ICP-MS	251±4	Gu et al., 2018
13	YZ02-49	E129°30′00″、N42°39′39″		石英闪长岩	LA-ICP-MS	251± 2	Zhang et al., 2004
14		E124°41′46″、N42°25′48″		流纹岩	SHRIMP	250±5	陈跃军等，2006
15	KY13-12	开原	佟家峪	高镁安山岩	SIMS	250±4	Yuan et al., 2016
16	DGTW03	E123°11′36″、N42°34′21″	腰窝堡	花岗质糜棱岩	SHRIMP	250±3	时溢，2020
17	CK66	E124°28′23″、N42°29′54″		花岗闪长岩	LA-ICP-MS	250±3	Gu et al., 2018
18	18FK037	法库东南	无名屯	辉长闪长岩	LA-ICP-MS	250±1	Jing et al., 2022
19	YZ02-2	E128°30′32″、N42°52′15″	大开	二长花岗岩	LA-ICP-MS	249±4	Zhang et al., 2004
20	14YB27-1	珲春	板石镇	英云闪长岩	LA-ICP-MS	249±6	杨东光，2018
21	FK04-24	法库	法库	花岗岩	SHRIMP	249±2	Zhang et al., 2010
22	HL-1	E129°10′08″、N42°35′20″		花岗岩	LA-ICP-MS	249±1	关庆彬等，2016
23	LK04-2	三门莫家	建平镇	二长花岗岩	LA-ICP-MS	249±1	曹花花，2013
24	13YB3-2	E128°52′20″、N42°46′13″	孟山	石英二长岩	LA-ICP-MS	249±1	Wang et al., 2015
25	18FK074	法库东南	小峰山	斜长角闪岩	LA-ICP-MS	249±1	Jing et al., 2022
26	18FK034	法库东南	富拉堡	闪长岩	LA-ICP-MS	249±1	Jing et al., 2022
27	14YB32	E130°15′01″、N42°43′18″		二长花岗岩	LA-ICP-MS	248±5	Yang et al., 2017
28	2930342	E126°28′05″、N43°07′55″	大屿山	花岗闪长岩	TIMS	248±4	孙德有等，2004
29	YZ02-27-2	E128°49′32″、N42°03′10″	百里坪	二长花岗岩	LA-ICP-MS	248±2	张艳斌等，2004
30	FK04-39	法库	法库	石英二长岩	SHRIMP	248±2	Zhang et al., 2010
31	18FK029	法库东南	二道沟	辉长闪长岩	LA-ICP-MS	248±1	Jing et al., 2022
32	18FK001	法库东南	红石砬子	辉长岩	LA-ICP-MS	248±2	Jing et al., 2022
33	18FK026	法库东南	前榆村	花岗岩	LA-ICP-MS	248±2	Jing et al., 2022
34	BJGC-TW1	E123°36′20″、N42°34′5″	柏家沟	花岗闪长岩	LA-ICP-MS	248±1	时溢等，2020
35	XFSTW1	E123°29′20″、N42°30′30″	晓峰山	闪长岩	LA-ICP-MS	248±1	Shi et al., 2022a
36	18FK039	法库东南	无名屯	花岗岩	LA-ICP-MS	248±1	Jing et al., 2022
37	18FK009	法库东南	红石砬子	辉长闪长岩	LA-ICP-MS	248±1	Jing et al., 2022
38	FW00-34	E127°53′47″、N43°08′45″	六棵松	闪长岩	SHRIMP	247±1	Wu et al., 2011
39	12LY2-1	E125°24′13″、N43°02′42″		黑云母二长岩	LA-ICP-MS	247±1	Cao et al., 2013
40	FK19001	法库东南	前榆村	辉绿岩	LA-ICP-MS	247±2	Jing et al., 2022
41	FK19004	法库东南	前榆村	花岗斑岩	LA-ICP-MS	247±1	Jing et al., 2022
42	FW00-110	E128°51′02″、N43°07′33″		二长花岗岩	TIMS	247±1	Wu et al., 2011
43	YZ02-40	E129°09′22″、N42°11′05″	柳东	花岗闪长岩	LA-ICP-MS	246±3	Wu et al., 2011
44	18FK020	法库东南	前榆村	辉长闪长岩	SIMS	246±3	Jing et al., 2022
45	JK5-1	E128°12′12″、N42°56′04″		角闪辉长岩	LA-ICP-MS	246±1	Wang et al., 2013
46	D2009	E124°34′24″、N42°27′48″	八棵树	辉长岩	LA-ICP-MS	246±2	本文
47	18FK033	法库东南	富拉堡	花岗岩	LA-ICP-MS	246±1	Jing et al., 2022
246~242Ma
48	YZ02-40	E129°09′22″、N42°11′05″		花岗闪长岩	LA-ICP-MS	246±3	Zhang et al., 2004
49	YZ02-22-2	E128°49′21″、N42°12′14″	百里坪	二长花岗岩	LA-ICP-MS	245±6	张艳斌等，2004
50	14YB33-1	E130°17′27″、N42°41′54″		英云闪长岩	LA-ICP-MS	245±4	Yang et al., 2017
51	YZ02-25-2	E128°44′58″、N42°10′57″	百里坪	二长花岗岩	LA-ICP-MS	245±3	张艳斌等，2004
52	14YB45	E130°24′31″、N42°39′52″	小盘岭	闪长岩	LA-ICP-MS	245±3	Yang et al., 2017
53	D6008TW1	E123°13′59″、N42°9′02″	雷其堡	二长花岗岩	SHRIMP	245±2	时溢，2020
54	13JH28-1	E128°57′31″、N42°45′59″	柳树沟	二长花岗岩	LA-ICP-MS	245±1	王子进，2016
55	LSSBTW1	E123°30′16″、N42°31′40″	灵山寺北	石英二长岩	LA-ICP-MS	245±1	Shi et al., 2022a
56		E125°17′16″、N43°17′34″		二长花岗岩	LA-ICP-MS	244±2	Wang et al., 2016
57	MG-28	E124°55′44″、N42°22′19″	松树咀	花岗闪长岩	SHRIMP	243±5	Wu et al., 2011
58	MG-103	E124°40′46″、N42°25′11″	尖山子	花岗闪长岩	SHRIMP	243±5	Wu et al., 2011
59	KLG	法库	靠陵沟	二长花岗岩	LA-ICP-MS	243±1	张超等，2021
60	b5157-1	E129°19′49″、N42°37′26″	永兴	二长花岗岩	LA-ICP-MS	243±1	关庆彬等，2016
242~240Ma
61	MG-64	E125°11′14″、N42°32′52″	小四坪	二长花岗岩	SHRIMP	242±7	Wu et al., 2011
62	XJP02	E124°48′23″、N42°20′07″	大甘河	二长花岗岩	LA-ICP-MS	242±1	Liu et al., 2020
63	FK04-5	E123°29′32″、N42°29′46″	法库	辉长岩	SHRIMP	241±6	Zhang et al., 2009
64	PM603-10-1	E123°13′58″、N42°18′06″	邦牛堡	花岗闪长岩	SHRIMP	241±2	时溢，2020
65	FQP	法库	凤岐堡	细粒花岗岩	LA-ICP-MS	241±1	张超等，2021
66	D0832-6	E130°59′51″、N43°15′27″	太平沟	高镁闪长岩	LA-ICP-MS	241±1	付长亮等，2010
67	FW00-122	E128°56′48″、N43°18′00″	西北岔	二长花岗岩	LA-ICP-MS	240±2	Wu et al., 2011
68	D0849-1	E130°53′17″、N43°12′52″	小西南岔	高镁闪长岩	LA-ICP-MS	240±1	付长亮等，2010
69	D2034	E124°22′35″、N42°32′01″	清河	流纹岩	LA-ICP-MS	241±2	本文
70	D2007	E124°25′49″、N42°31′51″	北大沟村	辉长岩	LA-ICP-MS	241±2	本文
240~230Ma
71	14YB34-1	珲春	板石镇	二云母花岗闪长岩	LA-ICP-MS	237±5	杨东光，2018
72	RZ22	E124°48′23″、N42°25′26″	宝兴	花岗闪长岩	LA-ICP-MS	235±2	刘锦等，2016
73	HL-5	E129°13′23″、N42°20′19″	南天	花岗闪长岩	LA-ICP-MS	235±1	关庆彬，2018
230~215Ma
74	D5121TW1	E123°16′34″、N42°31′31″	石洞沟	花岗岩	LA-ICP-MS	230±2	Shi et al., 2022a
75	FW00-50	E128°33′13″、N43°04′28″	青岭子	正长岩	LA-ICP-MS	229±3	Wu et al., 2011
76	07YB23	E128°32′49″、N43°04′35″	青岭子	辉长岩	LA-ICP-MS	229±2	Wu et al., 2011
77	YJT-1	E124°15′37″、N42°52′10″	余家屯	二长花岗岩	TIMS	229±1	辽宁省地质矿产勘查局，2003^①
78	07YB04	E128°45′33″、N43°16′21″	碱厂沟	正长岩	LA-ICP-MS	228±2	Wu et al., 2011
79	YB03-127	E130°31′16″、N44°23′14″	鸡冠砬子	二长花岗岩	LA-ICP-MS	227±4	Wu et al., 2011
80	D2503TW1	E123°04′11″、N42°31′10″	孙家屯	黑云母二长花岗岩	SHRIMP	227±2	时溢，2020
81	07YB36	E128°29′07″、N43°04′06″	二北青	正长岩	LA-ICP-MS	225±2	Wu et al., 2011
82	D2011	E124°17′59″、N42°22′35″	冰峪村	辉长岩	LA-ICP-MS	226±3	本文
83	RZ28	E124°51′26″、N42°26′00″	树德屯	辉长闪长岩	LA-ICP-MS	224±2	刘锦等，2016
84	14YB46-4	珲春	小盘岭	辉长岩	LA-ICP-MS	224±3	杨东光，2018
85	JEDG-4	E127°30′42″、N42°27′00″	二道沟	花岗闪长岩	SHRIMP	223±2	Miao et al., 2005
86	LK16-1		八棵树	方辉橄榄岩	SIMS	222±3	曹花花，2013
87	FX09-1		四家子	二长闪长岩	LA-ICP-MS	221±1	Zhang et al., 2012
88	FX09-11		四家子	花岗岩	LA-ICP-MS	221±2	Zhang et al., 2012
89	YZ02-43	E129°10′41″、N42°14′04″	柳东	石英闪长岩	LA-ICP-MS	220±2	Wu et al., 2011
90	DSL09-4		大烧楞	花岗闪长岩	LA-ICP-MS	219±2	Zhang et al., 2012
91	BJZ-3	E127°31′19″、N42°25′04″	百家子	石英正长岩	SHRMP	218±6	Miao et al., 2005
92	YB03-201	E129°44′15″、N43°43′05″	二岔子沟	正长花岗岩	LA-ICP-MS	218±2	Wu et al., 2011
93	FX09-2		四家子	花岗闪长岩	LA-ICP-MS	218±1	Zhang et al., 2012
94	99SW109	E126°25′22″、N42°53′52″	红旗岭	浅色辉长岩	SHRIMP	216±5	Wu et al., 2011
95	YB03-77	E130°44′52″、N44°08′49″	石河子	正长花岗岩	LA-ICP-MS	216±4	Wu et al., 2011
96	2859120	E127°46′13″、N43°53′37″	三道河	花岗岩	LA-ICP-MS	216±3	孙德有等，2005
97	FW00-86	E129°25′33″、N43°42′14″	春阳	二长花岗岩	TIMS	215±5	Wu et al., 2011

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华北板块北缘东段三叠纪构造演化——来自辽北开原岩浆岩年代学、地球化学的证据

作者简介: 陈井胜，1983年生，博士，教授级高级工程师，火成岩岩石学专业，E-mail: 5202268@qq.com

Evolution of the eastern segment of the northern margin of the North China Craton in the Triassic: Evidence from the geochronology and geochemistry of magmatic rocks in Kaiyuan area, North Liaoning

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作者简介:
陈井胜，1983年生，博士，教授级高级工程师，火成岩岩石学专业，E-mail: 5202268@qq.com