粤西晚侏罗世花岗质岩体及其暗色微粒包体的成因及意义：年代学、矿物学和地球化学约束

刘梓; 张玉芝; 崔翔; 甘成势; 王岳军

doi:10.3799/dqkx.2019.113

粤西晚侏罗世花岗质岩体及其暗色微粒包体的成因及意义：年代学、矿物学和地球化学约束

doi: 10.3799/dqkx.2019.113

刘梓^1, ,,
张玉芝^{1, 2, 3, ,},
崔翔^{1, 2, 3},
甘成势^{1, 2, 3},
王岳军^{1, 2, 3}

1.
中山大学地球科学与工程学院, 广东广州 510275
2.
广东省地球动力作用与地质灾害重点实验室, 广东广州 510275
3.
南方海洋科学与技术省实验室, 广东珠海 519082

基金项目:

国家自然科学基金项目 U1701641

中国科学技术部国家重点研发计划课题 2016YFC0600303

广东省自然科学基金项目 2018B030312007

详细信息

作者简介:
刘梓(1994-), 男, 硕士研究生, 构造地质学专业

通讯作者:
张玉芝

中图分类号: P59
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- 被引次数: 0
出版历程
- 收稿日期: 2019-05-19
- 刊出日期: 2020-04-15

Petrogenesis and Implications of the Late Jurassic Granitoid and Its Mafic Microgranular Enclaves in West Guangdong Province: Constraints from Geochronological, Mineralogical and Geochemical Evidence

Liu Zi^{1
,
,},
Zhang Yuzhi^{1, 2, 3
, ,},
Cui Xiang^{1, 2, 3},
Gan Chengshi^{1, 2, 3},
Wang Yuejun^{1, 2, 3}

1.
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275, China
2.
Guangdong Provincial Key Laboratory of Geodynamics and Geohazards, Guangzhou 510275, China
3.
Southern Laboratory of Ocean Science and Engineering, Zhuhai 519082, China

摘要

摘要: 粤西阳江市八二花岗质岩体中广泛发育似斑状细粒闪长质暗色微粒包体，这些暗色微粒包体形态多样，与寄主岩具相似的矿物组合，对研究花岗岩成因和壳-幔相互作用具有十分重要的意义.为了探讨它们的岩石成因及构造属性，对寄主岩和暗色微粒包体开展了系统的岩相学、年代学和地球化学研究.LA-ICP-MS锆石U-Pb定年结果表明，寄主岩年龄为160.0±1.0 Ma，暗色微粒包体年龄为159.3±1.1 Ma，均为晚侏罗世的产物.全岩地球化学特征显示，寄主岩属于富钾的准铝质I型花岗岩，寄主岩和暗色微粒包体均富集轻稀土元素和大离子亲石元素，亏损重稀土元素和Nb、Ta、Ti等高场强元素.此外，两者具相似的Sr-Nd同位素组成，寄主岩的ε_Nd（t）值为-5.73~-5.67，（⁸⁷Sr/⁸⁶Sr）_i值为0.707 63~0.707 67；而暗色微粒包体的ε_Nd（t）值为-5.81~-4.35，（⁸⁷Sr/⁸⁶Sr）_i值为0.707 04~0.707 74.锆石饱和温度计和角闪石全铝压力计表明八二花岗质岩体结晶于730~754℃和19.8~20.6 km.综合寄主岩及其暗色微粒包体的岩石学、地球化学、同位素特征，晚侏罗世八二花岗质岩体可能形成于陆内伸展背景，由于软流圈物质上涌底侵，导致中下地壳变基性岩为主的源岩部分熔融，并且源区有少量幔源物质的加入，局部可能存在岩浆混合作用；暗色微粒包体是由镁铁质岩浆与长英质岩浆混合形成的.
- 华南 /
- 晚侏罗世 /
- 暗色微粒包体 /
- U-Pb年龄 /
- 地球化学
Abstract: Mafic microgranular enclaves (MMEs) are widespread in the host granitoid from the Ba'er pluton in the west of the Guangdong Province. The MMEs have variable shapes and share similar mineral compositions with their host rocks, but are not fully understood. Petrographic study, zircon U-Pb dating and geochemical data are reported for the host granitoid and its MMEs, to constrain their petrogenesis and tectonic setting. LA-ICP-MS zircon U-Pb dating results yield weighted mean ²³⁸U/²⁰⁶Pb ages of 160.0±1.0 Ma and 159.3±1.1 Ma for the host rocks and the MMEs, respectively. The host granitoid is characterized by high SiO₂(61.04%-65.84%), K₂O(1.60%-4.97%), low A/CNK(1.59-1.99), belonging to metaluminous, K-enriched I-type granitoid. Both host rocks and MMEs are enriched in LREE and LILE, and are depleted in HREE and HFSE (e.g., Nb, Ta and Ti). In addition, they also have indistinguishable Sr-Nd isotopic compositions. The granitoid has ε_Nd(t) values of -5.73 to -5.67 and (⁸⁷Sr/⁸⁶Sr)_i values of 0.707 63-0.707 67. The MMEs have ε_Nd(t) values of -5.81 to -4.35 and (⁸⁷Sr/⁸⁶Sr)_i values of 0.707 04-0.707 74. The calculated crystallization temperatures and depths of the Ba'er pluton are 730-754℃ and 16.8-20.6 km, respectively. According to comprehensive analysis of their tectonic settings as well as petrographic characteristics and geochemical data, the magma produced by partial melting of predominantly mafic middle-lower crust, with the input of minor mantle-derived materials, experienced different degrees of fractional crystallization in an intraplate extensional setting of Late Jurassic, Southeast China, which was accompanied by local magma mixing. The MMEs are generated by the mixing of the mafic magma with felsic magma.
- South China /
- Late Jurassic /
- mafic microgranular enclave /
- U-Pb ages /
- geochemistry

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图 1 研究区地质简图与采样点

图a据Wang et al.(2003)；图b据广东省地质局（1964）1:20万地质图修改

Fig. 1. Geological schematic map of the study area and sample location

下载: 全尺寸图片幻灯片

图 2 寄主岩与MMEs野外照片

a.成群出现且大小不一的MMEs；b.纺锤状包体；c.双包体；d.寄主岩和MMEs交界处的长石斑晶

Fig. 2. Field photographs of host rocks and mafic microgranular enclaves

下载: 全尺寸图片幻灯片

图 3 寄主岩与MMEs典型岩相学显微照片

a.石英闪长岩显微照片；b.二长花岗岩显微照片；c.花岗闪长岩显微照片；d.MMEs发育典型岩浆结构；e.寄主岩中的角闪石等暗色矿物；f.MMEs中的针状磷灰石.矿物名称缩写：Qtz.石英；Pl.斜长石；Bi.黑云母；Amp.角闪石；Ap.磷灰石；Kfs.钾长石

Fig. 3. Photomicrographs of host rocks and mafic microgranular enclaves

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图 4 寄主岩(a)和MMEs(b)的锆石U-Pb年龄谐和图

Fig. 4. Zircon U-Pb concordia diagrams of host rocks (a) and mafic microgranular enclaves (b) from the Ba'er pluton

下载: 全尺寸图片幻灯片

图 5 寄主岩和MMEs的TAS(a)、A/CNK-A/NK(b)和SiO₂-K₂O(c)图解

图b据Maniar and Piccoli(1989)；图c据Rickwood(1989)

Fig. 5. TAS (a), A/NK-A/CNK(b) and SiO₂-K₂O(c) classification diagrams for the Ba'er pluton

下载: 全尺寸图片幻灯片

图 6 寄主岩(a，b)和MMEs(c，d)的球粒陨石标准化稀土元素配分图、原始地幔标准化微量元素蛛网图

球粒陨石、原始地幔数据引自Sun and McDonough (1989)

Fig. 6. Chondrite-normalized REE patterns and primitive mantle-normalized spidergrams of host rocks (a, b) and mafic microgranular enclaves (c, d)

下载: 全尺寸图片幻灯片

图 7 寄主岩和MMEs的哈克图解

Fig. 7. Harker diagrams of host granitoids and mafic microgranular enclaves

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图 8 MMEs中环带斜长石的背散射图像(a)和电子探针数据(b)；寄主岩中环带斜长石的背散射图像(c)和电子探针数据(d)

An为钙长石牌号

Fig. 8. Back-scattered electron images of zoned plagioclases (a, c) and EPMA data of the plagioclase component (b, d) of host rocks and MMEs, respectively

下载: 全尺寸图片幻灯片

图 9 寄主岩及其MMEs(⁸⁷Sr/⁸⁶Sr)_i-ε_Nd(t)图解

晚侏罗世花岗岩数据引自Li et al.(2007)，Xu et al.(2007); 晚侏罗世基性岩数据引自Meng et al. (2012)，Wang et al.(2003, 2008)，Gan et al.(2018)

Fig. 9. (⁸⁷Sr/⁸⁶Sr)_i-ε_Nd(t) diagram of granodiorites and enclaves in the Ba'er pluton

下载: 全尺寸图片幻灯片

图 10 不同源岩脱水部分熔融实验获得的熔体图解

a, b据Wang et al. (2016)

Fig. 10. Experimental results of partial melts from different source rock types

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图 11 Th_N/Yb_N-Nb_N/Th_N关系图(a)和MgO-FeO_t图(b)

图a据曾认宇等(2016)；图b据Zorpi et al.(1989)

Fig. 11. Diagrams of Th_N/Yb_N-Nb_N/Th_N (a) and MgO-FeO_t (b)

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表 1 暗色微粒包体及寄主岩锆石LA-MC-ICP-MS锆石U-Pb定年结果

Table 1. LA-MC-ICP-MS U-Pb zircon data of host rocks and MMEs in the Ba'er pluton

样品	同位素比值						年龄(Ma)
样品	²⁰⁷Pb/ ²⁰⁶Pb	1σ	²⁰⁷Pb/ ²³⁵U	1σ	²⁰⁶Pb/ ²³⁸U	1σ	²⁰⁷Pb/ ²⁰⁶Pb	1σ	²⁰⁷Pb/ ²³⁵U	1σ	²⁰⁶Pb/ ²³⁸U	1σ	谐和度
暗色微粒包体
15YD-01-01	0.048 75	0.001 73	0.171 43	0.005 48	0.025 20	0.000 80	200	83	161	5	160	5	99%
15YD-01-02	0.048 44	0.001 68	0.169 34	0.005 52	0.025 05	0.000 81	121	88	159	5	160	5	99%
15YD-01-03	0.050 57	0.001 73	0.175 49	0.005 56	0.024 96	0.000 79	220	80	164	5	159	5	96%
15YD-01-04	0.062 78	0.002 16	0.235 91	0.008 60	0.027 07	0.000 89	702	69	215	7	172	6	77%
15YD-01-05	0.048 68	0.001 59	0.171 59	0.006 36	0.025 31	0.000 93	132	76	161	6	161	6	99%
15YD-01-06	0.056 48	0.002 00	0.195 18	0.007 86	0.024 54	0.000 87	472	78	181	7	156	6	85%
15YD-01-07	0.049 12	0.001 57	0.170 61	0.005 59	0.025 03	0.000 81	154	79	160	5	159	5	99%
15YD-01-08	0.050 64	0.001 57	0.176 22	0.005 67	0.025 05	0.000 80	233	72	165	5	160	5	96%
15YD-01-09	0.048 92	0.001 50	0.171 27	0.005 54	0.025 24	0.000 81	143	68	161	5	161	5	99%
15YD-01-10	0.049 35	0.001 51	0.173 05	0.005 67	0.025 31	0.000 83	165	68	162	5	161	5	99%
15YD-01-11	0.055 85	0.001 72	0.236 32	0.007 67	0.030 77	0.001 02	456	73	215	6	195	6	90%
15YD-01-12	0.049 60	0.001 50	0.170 01	0.005 74	0.024 76	0.000 83	176	75	159	5	158	5	98%
15YD-01-13	0.049 52	0.001 51	0.169 98	0.005 62	0.024 85	0.000 81	172	72	159	5	158	5	99%
15YD-01-14	0.051 21	0.001 54	0.174 78	0.006 14	0.024 72	0.000 87	250	64	164	5	157	6	96%
15YD-01-15	0.050 77	0.001 58	0.173 91	0.005 70	0.024 86	0.000 79	232	68	163	5	158	5	97%
15YD-01-16	0.051 46	0.001 63	0.176 06	0.005 72	0.024 86	0.000 78	261	72	165	5	158	5	96%
15YD-01-17	0.052 49	0.001 60	0.177 49	0.005 91	0.024 47	0.000 78	306	70	166	5	156	5	93%
15YD-01-18	0.048 62	0.001 50	0.168 70	0.005 52	0.025 26	0.000 83	128	79	158	5	161	5	98%
15YD-01-19	0.048 39	0.001 48	0.168 50	0.005 39	0.025 34	0.000 81	117	72	158	5	161	5	97%
15YD-01-20	0.051 52	0.001 63	0.175 91	0.006 10	0.024 70	0.000 79	265	77	165	5	157	5	95%
15YD-01-21	0.049 32	0.001 50	0.170 00	0.005 39	0.025 02	0.000 78	165	66	159	5	159	5	99%
15YD-01-22	0.050 12	0.001 55	0.174 11	0.006 77	0.025 15	0.000 94	211	103	163	6	160	6	98%
15YD-01-23	0.051 20	0.001 57	0.176 91	0.005 67	0.025 04	0.000 78	250	72	165	5	159	5	96%
15YD-01-24	0.049 35	0.001 52	0.170 99	0.005 61	0.025 09	0.000 79	165	68	160	5	160	5	99%
15YD-01-25	0.049 51	0.001 55	0.171 77	0.005 75	0.025 14	0.000 81	172	72	161	5	160	5	99%
寄主岩
15YD-02-01	0.049 51	0.001 50	0.172 49	0.005 95	0.025 21	0.000 87	172	72	162	5	161	6	99%
15YD-02-02	0.049 25	0.001 49	0.170 60	0.005 68	0.025 07	0.000 83	167	70	160	5	160	5	99%
15YD-02-03	0.049 61	0.001 51	0.172 01	0.006 03	0.025 11	0.000 87	176	75	161	5	160	6	99%
15YD-02-04	0.049 74	0.001 50	0.171 74	0.005 57	0.024 98	0.000 81	183	70	161	5	159	5	98%
15YD-02-05	0.049 53	0.001 49	0.171 95	0.005 50	0.025 13	0.000 80	172	70	161	5	160	5	99%
15YD-02-06	0.049 67	0.001 50	0.173 23	0.005 41	0.025 25	0.000 78	189	73	162	5	161	5	99%
15YD-02-07	0.048 95	0.001 49	0.170 42	0.005 71	0.025 19	0.000 84	146	72	160	5	160	5	99%
15YD-02-08	0.049 65	0.001 52	0.175 23	0.006 61	0.025 35	0.000 90	189	75	164	6	161	6	98%
15YD-02-09	0.050 96	0.001 54	0.175 56	0.006 02	0.025 05	0.000 87	239	69	164	5	160	6	97%
15YD-02-10	0.049 54	0.001 49	0.173 01	0.005 56	0.025 31	0.000 81	172	70	162	5	161	5	99%
15YD-02-11	0.049 24	0.001 51	0.170 56	0.005 55	0.025 11	0.000 80	167	70	160	5	160	5	99%
15YD-02-12	0.049 42	0.001 49	0.171 24	0.005 71	0.025 14	0.000 84	169	70	161	5	160	5	99%
15YD-02-13	0.059 55	0.001 89	0.201 13	0.007 03	0.024 45	0.000 81	587	69	186	6	156	5	82%
15YD-02-14	0.049 14	0.001 49	0.170 14	0.005 52	0.025 13	0.000 81	154	75	160	5	160	5	99%
15YD-02-15	0.049 67	0.001 56	0.172 44	0.005 68	0.025 23	0.000 80	189	72	162	5	161	5	99%
15YD-02-16	0.049 50	0.001 49	0.172 66	0.005 76	0.025 32	0.000 84	172	70	162	5	161	5	99%
15YD-02-17	0.048 88	0.001 62	0.167 92	0.005 85	0.025 09	0.000 83	143	78	158	5	160	5	98%
15YD-02-18	0.049 98	0.001 52	0.173 58	0.005 80	0.025 26	0.000 84	195	72	163	5	161	5	98%
15YD-02-19	0.049 24	0.001 48	0.169 73	0.005 47	0.025 05	0.000 81	167	70	159	5	160	5	99%
15YD-02-20	0.049 38	0.001 49	0.171 95	0.005 72	0.025 30	0.000 84	165	68	161	5	161	5	99%
15YD-02-21	0.049 65	0.001 50	0.171 56	0.005 70	0.025 09	0.000 82	189	75	161	5	160	5	99%
15YD-02-22	0.049 56	0.001 50	0.171 71	0.005 86	0.025 18	0.000 85	176	70	161	5	160	5	99%
15YD-02-23	0.050 87	0.001 56	0.175 94	0.005 91	0.025 10	0.000 83	235	72	165	5	160	5	97%
15YD-02-24	0.049 24	0.001 49	0.171 56	0.005 61	0.025 26	0.000 82	167	70	161	5	161	5	99%
15YD-02-25	0.049 77	0.001 51	0.172 53	0.006 02	0.025 16	0.000 88	183	66	162	5	160	6	99%

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表 2 暗色微粒包体及寄主岩主量元素(%)、微量元素(10^-6)和Sr-Nd同位素组成分析结果

Table 2. Major oxides (%), trace elements (10^-6) and Sr-Nd isotopic results of host rocks and MMEs in the Ba'er pluton

样品	YD-01C	YD-01D	YD-01E	YD-01F	YD-01G	YD-02A	YD-02B	YD-02C	YD-02D	YD-02E
岩性	暗色微粒包体					寄主岩
SiO₂	55.53	57.08	56.44	55.26	56.42	65.84	63.94	61.04	65.98	63.73
TiO₂	1.29	1.16	1.22	1.12	1.25	0.74	0.55	0.98	0.72	0.66
Al₂O₃	17.83	17.36	17.37	16.83	17.23	15.10	16.81	16.07	15.47	16.34
CaO	6.50	6.18	6.42	6.99	6.50	4.54	3.47	4.81	4.52	3.87
FeO_t	8.68	8.15	8.46	8.54	8.55	5.69	4.62	7.41	5.28	5.42
K₂O	2.04	1.79	1.80	2.25	1.76	1.60	4.97	2.34	1.79	3.97
MgO	2.79	2.84	2.96	4.02	2.98	1.85	1.51	2.45	1.68	1.71
MnO	0.14	0.16	0.16	0.21	0.17	0.11	0.09	0.14	0.10	0.10
Na₂O	3.91	3.93	3.93	3.33	3.90	3.56	3.17	3.56	3.66	3.34
P₂O₅	0.29	0.27	0.30	0.27	0.30	0.23	0.18	0.30	0.21	0.21
LOI	0.70	0.79	0.64	0.89	0.66	0.49	0.41	0.61	0.33	0.37
Total	99.70	99.71	99.70	99.70	99.70	99.73	99.72	99.72	99.73	99.72
Mg^#	43	45	45	52	45	43	43	43	43	42
A/CNK	0.87	0.88	0.86	0.82	0.86	0.95	1.00	0.94	0.96	0.97
A/NK	2.06	2.07	2.06	2.13	2.07	1.99	1.59	1.91	1.95	1.67
Li	85.01	91.64	88.74	75.77	82.12	77.96	60.77	95.46	64.63	61.73
Be	2.28	2.29	3.11	3.90	2.41	4.02	3.64	4.17	3.86	3.98
Sc	20.23	18.79	21.05	22.12	19.19	13.01	11.32	16.69	12.36	12.67
V	214.08	186.56	192.97	189.19	193.03	100.51	85.71	129.97	95.80	97.29
Cr	11.31	12.41	7.26	34.95	8.09	13.23	16.95	20.55	10.37	11.47
Co	22.67	22.00	21.59	24.81	22.17	12.57	9.74	16.57	11.68	11.57
Ni	6.60	7.64	6.34	17.83	6.57	6.25	5.51	13.64	5.45	4.82
Cu	21.38	28.47	27.31	28.20	28.68	11.03	6.56	12.16	6.68	7.13
Zn	145.90	143.76	144.54	133.97	138.40	97.36	82.46	123.55	88.49	87.27
Ga	21.94	21.40	21.01	20.86	20.80	19.81	17.66	21.02	19.40	18.30
Rb	127.99	149.81	145.66	120.19	138.23	113.00	167.92	158.16	119.28	163.05
Sr	516.70	440.97	446.41	428.97	441.45	383.59	445.22	390.81	397.78	431.19
Y	31.06	27.91	29.88	33.07	31.34	27.31	16.68	32.46	27.77	21.26
Zr	231.07	222.79	198.25	163.96	210.34	234.43	201.91	303.35	212.46	207.94
Nb	13.67	13.00	14.33	16.70	14.61	15.02	9.63	18.94	14.76	12.07
Cs	9.34	11.82	11.30	6.88	11.26	8.01	8.33	11.15	9.36	9.70
Ba	538.47	240.85	316.04	461.07	253.69	150.31	1064.07	284.51	200.39	720.25
La	38.32	45.51	45.36	27.14	42.23	60.87	32.81	47.87	40.86	39.56
Ce	77.87	84.96	87.67	61.15	85.01	109.52	61.45	95.27	76.19	70.96
Pr	9.24	9.16	10.03	7.46	9.84	11.36	6.26	10.72	8.51	7.66
Nd	34.37	34.09	36.49	30.41	37.33	37.30	21.95	38.62	29.75	24.74
Sm	6.86	6.00	7.10	6.62	7.19	6.71	3.57	6.98	5.78	4.67
Eu	1.70	1.49	1.70	1.48	1.70	1.37	0.91	1.61	1.29	1.06
Gd	6.54	5.98	6.70	6.51	6.73	5.99	3.30	6.69	5.32	3.72
Tb	0.97	0.90	0.99	0.96	1.03	0.92	0.50	1.03	0.82	0.63
Dy	5.19	4.74	5.30	5.49	5.50	4.59	2.61	5.78	4.38	3.21
Ho	1.01	0.90	1.03	1.08	1.06	0.92	0.56	1.12	0.87	0.62
Er	2.89	2.65	2.92	3.16	2.97	2.69	1.58	3.16	2.50	1.95
Tm	0.41	0.35	0.40	0.46	0.40	0.39	0.23	0.46	0.35	0.28
Yb	2.53	2.22	2.56	3.05	2.64	2.47	1.49	3.02	2.38	1.83
Lu	0.38	0.34	0.40	0.45	0.39	0.39	0.24	0.45	0.36	0.30
Hf	5.21	5.02	4.74	3.88	5.11	5.90	4.93	7.68	4.89	4.80
Ta	0.80	0.75	0.95	0.85	1.26	1.77	0.95	2.02	1.69	1.16
W	1.04	0.86	0.73	1.13	1.42	0.50	0.77	1.13	0.66	0.51
Tl	0.64	0.76	0.77	0.60	0.76	0.61	0.84	0.88	0.59	0.76
Pb	12.92	14.15	14.65	12.71	14.77	14.00	26.35	14.71	13.48	19.56
Bi	0.21	0.25	0.26	0.19	0.23	0.24	0.18	0.22	0.22	0.19
Th	8.82	10.92	10.70	6.77	10.35	25.51	16.23	22.35	17.88	16.96
U	2.06	2.54	2.77	1.93	2.46	6.35	4.60	6.72	5.25	4.77
Eu*	0.78	0.76	0.75	0.69	0.75	0.66	0.81	0.72	0.71	0.78
T_zr(℃)						746	732	754	737	730
∑REE	188.28	199.29	208.66	155.41	204.01	245.49	137.46	222.78	179.34	161.20
LREE	168.35	181.21	188.36	134.27	183.29	227.13	126.96	201.07	162.37	148.65
HREE	19.92	18.07	20.30	21.14	20.71	18.36	10.50	21.71	16.97	12.55
LREE/HREE	8.45	10.03	9.28	6.35	8.85	12.37	12.09	9.26	9.57	11.85
(La/Yb)_N	10.85	14.73	12.70	6.39	11.47	17.67	15.80	11.38	12.29	15.47
Rb/Sr	0.25	0.34	0.33	0.28	0.31	0.29	0.38	0.40	0.30	0.38
Nb/Ta	17.2	17.3	15.0	19.7	11.6	8.5	10.1	9.4	8.7	10.4
⁸⁷Rb/⁸⁶Sr	0.436 34			0.983 16		0.852 46			0.867 79
¹⁴⁷Sm/¹⁴⁴Nd	0.100 26			0.106 47		0.108 69			0.117 38
⁸⁷Sr/⁸⁶Sr	0.708 02			0.709 93		0.709 54			0.709 60
2σ	0.000 008			0.000 008		0.000 006			0.000 006
¹⁴³Nd/¹⁴⁴Nd	0.512 316			0.512 247		0.512 254			0.512 266
2σ	0.000 006			0.000 005		0.000 003			0.000 006
（⁸⁷Sr/⁸⁶Sr）_i	0.707 04			0.707 74		0.707 63			0.707 67
ε_Nd(t)	-4.35			-5.81		-5.73			-5.67
T_DM² (Ga)	1.12			1.28		1.30			1.40
注：LOI.烧失量; A/NK(摩尔比)=Al₂O₃/(Na₂O+K₂O); A/CNK(摩尔比)=Al₂O₃/(Na₂O+K₂O+CaO); Eu*=Eu_N/[(Sm_N×Gd_N)^1/2]; (⁸⁷Sr/⁸⁶Sr)_i=(⁸⁷Sr/⁸⁶Sr)_S-(⁸⁷Rb/⁸⁶Sr)_S×(e^λt-1); λ=1.42×10^-11 a^-1; ε_Sr=[(¹⁴³Nd/¹⁴⁴Nd)_S/(¹⁴³Nd/¹⁴⁴Nd)_CHUR-1]×10 000; ε_Nd=[(¹⁴³Nd/¹⁴⁴Nd)_S/(¹⁴³Nd/¹⁴⁴Nd)_CHUR-1]×10 000; t代表样品形成时间，S代表样品，CHUR代表球粒陨石; (¹⁴⁷Sm/¹⁴⁴Nd)_CHUR=0.196 7; (¹⁴³Nd/¹⁴⁴Nd)_CHUR=0.512 638

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表 3 暗色微粒包体和寄主岩中斜长石的电子探针数据（%）

Table 3. EMPA results (%) of plagioclases in MMEs and host rocks

Samples	SiO₂	TiO₂	Al₂O₃	FeO	MnO	MgO	CaO	Na₂O	K₂O	Total	Si	Al	Ca	Na	K	Or	Ab	An
暗色微粒包体
15YD-01-2-1	59.54	0.00	25.10	0.08	0.00	0.00	6.91	7.69	0.14	99.47	2.67	1.33	0.33	0.67	0.01	0.80	66.28	32.91
15YD-01-2-2	59.30	0.00	24.64	0.16	0.04	0.00	7.01	7.62	0.15	98.91	2.68	1.31	0.34	0.67	0.01	0.86	65.73	33.42
15YD-01-2-3	59.78	0.02	25.41	0.03	0.01	0.00	7.11	7.57	0.17	100.10	2.66	1.33	0.34	0.65	0.01	0.96	65.18	33.86
15YD-01-2-4	59.24	0.03	25.06	0.10	0.01	0.00	7.30	7.50	0.19	99.42	2.66	1.33	0.35	0.65	0.01	1.06	64.35	34.60
15YD-01-2-5	58.86	0.00	25.46	0.09	0.01	0.02	7.38	7.82	0.20	99.83	2.64	1.35	0.35	0.68	0.01	1.07	65.01	33.91
15YD-01-2-6	59.87	0.00	25.14	0.15	0.02	0.01	6.97	7.68	0.23	100.06	2.67	1.32	0.33	0.66	0.01	1.31	65.71	32.98
15YD-01-2-7	59.04	0.00	24.81	0.16	0.02	0.02	7.05	7.55	0.19	98.84	2.67	1.32	0.34	0.66	0.01	1.07	65.25	33.68
15YD-01-3-1	59.55	0.00	25.32	0.00	0.00	0.00	7.42	7.80	0.19	100.28	2.65	1.33	0.35	0.67	0.01	1.01	64.87	34.12
15YD-01-3-2	58.98	0.00	25.41	0.10	0.00	0.01	7.49	7.39	0.23	99.60	2.65	1.34	0.36	0.64	0.01	1.31	63.25	35.44
15YD-01-3-3	56.90	0.00	26.59	0.11	0.00	0.00	8.83	6.60	0.12	99.15	2.57	1.42	0.43	0.58	0.01	0.69	57.10	42.21
15YD-01-3-4	58.57	0.00	26.38	0.10	0.00	0.00	8.08	7.05	0.11	100.29	2.61	1.39	0.39	0.61	0.01	0.62	60.85	38.54
15YD-01-3-5	59.36	0.00	25.34	0.11	0.00	0.03	7.31	7.60	0.12	99.87	2.65	1.34	0.35	0.66	0.01	0.68	64.86	34.46
15YD-01-3-6	59.10	0.00	25.31	0.14	0.01	0.01	7.56	7.66	0.14	99.92	2.65	1.34	0.36	0.66	0.01	0.77	64.19	35.04
15YD-01-3-7	59.17	0.00	25.14	0.07	0.00	0.00	7.39	7.67	0.12	99.56	2.66	1.33	0.36	0.67	0.01	0.64	64.83	34.53
15YD-01-3-8	60.55	0.00	24.75	0.16	0.04	0.01	6.41	8.30	0.15	100.37	2.69	1.30	0.31	0.71	0.01	0.83	69.50	29.67
寄主岩
15YD-02-2-1	60.53	0.07	24.63	0.05	0.00	0.00	6.46	8.11	0.12	99.98	2.70	1.29	0.31	0.70	0.01	0.69	68.98	30.34
15YD-02-2-2	60.60	0.01	24.65	0.09	0.00	0.00	6.39	8.16	0.18	100.08	2.70	1.29	0.30	0.70	0.01	0.99	69.13	29.88
15YD-02-2-3	60.45	0.00	24.62	0.00	0.02	0.00	6.50	8.06	0.15	99.79	2.70	1.29	0.31	0.70	0.01	0.84	68.60	30.56
15YD-02-2-4	58.32	0.00	25.68	0.15	0.05	0.01	8.18	7.28	0.15	99.83	2.62	1.36	0.39	0.63	0.01	0.85	61.17	37.98
15YD-02-2-5	57.86	0.00	26.22	0.05	0.00	0.02	8.37	6.83	0.14	99.50	2.60	1.39	0.40	0.60	0.01	0.81	59.16	40.03
15YD-02-2-6	57.97	0.01	26.03	0.06	0.03	0.00	8.28	6.98	0.11	99.48	2.61	1.38	0.40	0.61	0.01	0.63	60.03	39.35
15YD-02-2-7	58.57	0.00	25.82	0.02	0.00	0.04	7.46	7.28	0.09	99.28	2.63	1.37	0.36	0.63	0.00	0.50	63.53	35.97
15YD-02-2-8	59.75	0.00	25.05	0.15	0.01	0.00	7.01	7.45	0.12	99.54	2.67	1.32	0.34	0.65	0.01	0.68	65.34	33.99
15YD-02-1-1	59.78	0.01	25.01	0.06	0.00	0.00	7.09	7.90	0.07	99.92	2.67	1.32	0.34	0.68	0.00	0.39	66.59	33.02
15YD-02-1-2	59.59	0.00	25.16	0.04	0.00	0.04	7.03	7.65	0.13	99.65	2.67	1.33	0.34	0.66	0.01	0.76	65.82	33.42
15YD-02-1-3	58.44	0.01	25.92	0.09	0.00	0.00	7.93	7.31	0.11	99.81	2.62	1.37	0.38	0.64	0.01	0.62	62.13	37.25
15YD-02-1-4	58.61	0.00	26.22	0.00	0.00	0.00	7.96	7.20	0.08	100.07	2.62	1.38	0.38	0.62	0.00	0.47	61.78	37.74
15YD-02-1-5	60.38	0.03	24.61	0.01	0.12	0.03	6.64	7.99	0.09	99.88	2.69	1.29	0.32	0.69	0.00	0.49	68.22	31.30
15YD-02-2-1	58.49	0.00	25.96	0.01	0.00	0.00	7.95	6.93	0.09	99.43	2.63	1.37	0.38	0.60	0.01	0.51	60.91	38.58
15YD-02-1-2	58.78	0.01	26.02	0.02	0.01	0.00	7.82	7.18	0.15	99.97	2.63	1.37	0.37	0.62	0.01	0.85	61.88	37.27
15YD-02-1-3	59.24	0.04	25.56	0.11	0.00	0.00	7.70	7.46	0.19	100.29	2.64	1.34	0.37	0.64	0.01	1.08	63.00	35.93

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表 4 暗色微粒包体和寄主岩中角闪石电子探针分析结果(%)

Table 4. EMPA results(%) of hornblendes in enclaves and host rocks

Samples	15YD- 01-2-1	15YD- 01-2-2	15YD- 01-3-1	15YD- 01-3-2	15YD- 02-2-1	15YD- 02-2-2
Samples	暗色微粒包体				寄主岩
SiO₂	42.24	42.36	42.41	42.28	41.99	42.27
TiO₂	0.85	0.86	0.91	0.92	0.83	0.84
Al₂O₃	10.46	10.66	10.53	10.71	10.98	10.81
FeO	20.74	20.22	20.87	20.39	21.13	21.28
MnO	0.60	0.64	0.52	0.51	0.55	0.78
MgO	8.12	8.58	8.25	8.50	8.05	7.96
CaO	11.36	11.56	11.59	11.71	11.52	11.63
Na₂O	0.32	0.41	0.39	0.36	0.33	0.32
K₂O	1.32	1.17	1.41	1.18	1.06	1.22
以23个O计算的阳离子数
Si	6.45	6.42	6.43	6.41	6.37	6.39
Al ^IV	1.55	1.58	1.57	1.59	1.63	1.61
Al ^VI	0.33	0.32	0.32	0.32	0.33	0.32
Ti	0.10	0.10	0.10	0.11	0.10	0.10
Fe³⁺	0.96	0.96	0.89	0.92	1.06	1.00
Fe²⁺	1.69	1.60	1.76	1.66	1.62	1.69
Mn	0.08	0.08	0.07	0.07	0.07	0.10
Mg	1.85	1.94	1.87	1.92	1.82	1.80
Ca	1.86	1.88	1.88	1.90	1.87	1.88
Na	0.09	0.12	0.11	0.11	0.10	0.09
K	0.26	0.23	0.27	0.23	0.20	0.23
P (kbar)	5.94	6.05	5.95	6.10	6.34	6.16
H (km)	19.63	20.12	19.62	19.96	20.91	20.32

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