东南极Windmill群岛与罗迪尼亚超大陆聚合相关构造热事件的时代：来自Bailey半岛镁铁质片麻岩和淡色片麻岩锆石SHRIMP U-Pb年龄的约束

王彦斌; 王浩; 任留东; 焦永艳; 仝来喜; WILLIAMSIan S

doi:10.12090/j.issn.1006-6616.2021.27.05.063

东南极Windmill群岛与罗迪尼亚超大陆聚合相关构造热事件的时代：来自Bailey半岛镁铁质片麻岩和淡色片麻岩锆石SHRIMP U-Pb年龄的约束

doi: 10.12090/j.issn.1006-6616.2021.27.05.063

1.
中国地质科学院地质研究所北京离子探针中心, 北京 100037
2.
西北大学地质学系大陆动力学国家实验室, 陕西西安 710069
3.
Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia

基金项目:

国家自然科学基金项目 40773042

国家自然科学基金项目 41073014

国家自然科学基金项目 41373052

国家自然科学基金项目 41773049

国家海洋局极地考察办公室对外合作项目 CHINARE-IC201707

详细信息

作者简介:
王彦斌(1966-), 男, 博士, 研究员, 从事同位素地质年代学和地球化学研究工作。E-mail: wangyanbin@bjshrimp.cn

中图分类号: P597.3
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- 被引次数: 0
出版历程
- 收稿日期: 2021-06-28
- 修回日期: 2021-08-23
- 预出版日期: 2021-12-31
- 刊出日期: 2021-10-28

Zircon U-Pb ages of the mafic gneiss and leucogneiss from the Bailey Peninsula: Constraints on the timing of the tectonothermal events related to the amalgamation of Rodinia in the Windmill Islands, East Antarctica

1.
Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, Shaanxi, China
3.
Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia

Funds:

the National Natural Science Foundation of China 40773042

the National Natural Science Foundation of China 41073014

the National Natural Science Foundation of China 41373052

the National Natural Science Foundation of China 41773049

the Polar Office of the State Oceanic Bureau of China CHINARE-IC201707

摘要

摘要: 东南极Windmill群岛变质杂岩经历的变质和岩浆事件与西澳大利亚Albany-Fraser造山带在时间上相对应，并可能与罗迪尼亚超大陆的拼合有关。Windmill群岛Bailey半岛的镁铁质片麻岩(角闪石-单斜辉石-斜方辉石-黑云母-斜长石-石英-磁铁矿-锆石)被认为具有较早的形成年龄，其中还出露属于正片麻岩的淡色片麻岩(斜长石-钾长石-石英-黑云母-锆石)。对这两种片麻岩中的锆石分别进行了SHRIMP U-Pb年龄测定，首次获得该区镁铁质片麻岩锆石核部²⁰⁷Pb/²⁰⁶Pb加权平均年龄1403±28 Ma，该年龄记录了本区中元古代早期岩浆事件，这是Windmill群岛地区记录的最早一期岩浆事件，可能受到了东部莫森大陆(Mawson Continent)构造岩浆活动的影响。铁镁质片麻岩锆石增生边的年龄为1318±34 Ma，则记录了早期构造热事件。淡色片麻岩中锆石核部年龄为1257±51 Ma，与Bailey半岛的片麻状含石榴子石花岗岩侵位年龄一致，共同记录了该区的一期岩浆活动。淡色片麻岩中锆石增生边的年龄为1197±26 Ma，记录了晚期的变质事件。这些新的年龄数据强烈支持1375~1151 Ma期间东南极Windmill群岛与西澳大利亚Albany-Fraser造山带相连接的构造模型，同时也为罗迪尼亚超大陆拼合过程提供了重要的年代学约束。
- SHRIMP锆石U-Pb年龄 /
- 镁铁质片麻岩 /
- 淡色片麻岩 /
- Windmill群岛 /
- 东南极 /
- 罗迪尼亚
Abstract: We report new geochronological data of the mafic gneiss and leucogneiss from the Windmill Islands, East Antarctica, in order to unravel the tectonothermal events related to the amalgamation of Rodinia. SHRIMP zircon U-Pb dating from the mafic gneiss (Hbl-Cpx-Opx-Bt-Pl-Qtz-Mag-Zrn) yielded early Mesoproterozoic magmatic ages of 1403±28 Ma from igneous cores, and middle Mesoproterozoic metamorphic ages of 1318±34 Ma from overgrown rims. The leucogneiss (Pl-Kfs-Qtz-Bt-Zrn) in the Bailey Peninsula has intrusive ages of 1257±51 Ma from magmatic origin zircon cores, and metamorphic ages of 1197±26 Ma from overgrown rims and/or structureless grains. The intrusive age of mafic gneiss indicates the existence of a ca.1.40 Ga igneous activity in the Windmill Islands. This is likely the earliest igneous record of the Windmill Islands, possibly relating to the final period of igneous activity of the Mawson Continent. The age of high-grade metamorphism of the mafic gneiss from the Bailey Peninsula can be constrained by the metamorphic zircon overgrowth at 1318±34 Ma, suggesting that the Windmill Islands was possibly involved in the Albany-Fraser-Windmill (East Antarctic) orogeny during the 1375~1151 Ma period. This study further supports the tectonic model in which the Windmill Islands and the Albany-Fraser Orogeny are parallel convergence during the Mesoproterozoic Rodinia amalgamation.
- SHRIMP zircon U-Pb ages /
- mafic gneiss /
- leucogneiss /
- Windmill Islands /
- East Antarctica /
- Rodinia

HTML全文

图 1 Windmill群岛地质简图(据Zhang et al., 2012修改)

a、b-Windmill群岛在南极的位置；c-Windmill群岛北部地质简图

Figure 1. Sketch geological map of the Windmill Islands (modified after Zhang et al., 2012)

(a and b) Location of the Windmill Islands in Antarctica; (c)Sketch geological map of the northern part of the Windmill Islands

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图 2 Bailey半岛地质简图(据Paul et al., 1995修改)

Figure 2. Geological map of the Bailey Peninsula (modified after Paul et al., 1995)

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图 3 Bailey半岛镁铁质片麻岩和淡色片麻岩显微镜下照片

Hbl-角闪石；Opx-斜方辉石；Cpx-单斜辉石；Bt-黑云母；Pl-斜长石；Qtz-石英；Mag-磁铁矿; Kfs-钾长石
a-镁铁质片麻岩(C0121-1)，单偏光；b-镁铁质片麻岩(C0121-1)，正交偏光；c-淡色片麻岩(C0121-2)，单偏光；d-淡色片麻岩(C0121-2)，正交偏光

Figure 3. Micrographs showing petrographic features of the mafic gneiss and leucogneiss in the Bailey Peninsula, Windmill Islands

(a)Plane-polarized light image of mafic gneiss; (b)Cross-polarized light image of mafic gneiss; (c)Plane-polarized light image of leucogneiss; (d)Cross-polarized light image of leucogneiss
Hbl-hornblende; Opx-orthopyroxene; Cpx-clinopyroxene; Bt-biotite; Pl-plagioclase; Qtz-quartz; Mag-magnetite; Kfs-K-feldspar

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图 4 Bailey半岛镁铁质片麻岩和淡色片麻岩样品锆石透射光和阴极发光图像

a-镁铁质片麻岩(C0121-1)；b-淡色片麻岩样品(C0121-2)

Figure 4. Characteristic images of the analyzed zircons from the mafic gneiss and leucogneiss in the Bailey Peninsula

(a) The mafic gneiss sample (C0121-1); (b) The leucogneiss sample (C0121-2)

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图 5 Bailey半岛镁铁质片麻岩样品锆石U-Pb谐和图

Figure 5. U-Pb concordia diagram of zircons from the mafic gneiss in the Bailey Peninsula

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图 6 Bailey半岛淡色片麻岩样品锆石U-Pb谐和图

Figure 6. U-Pb concordia diagram of the zircons from the leucogneiss in the Bailey Peninsula

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图 7 南极洲和澳大利亚的冈瓦纳大陆构造图(据Liu et al., 2018修改)

AFO-Albany-Fraser造山带；BH-Bunger丘陵；CCr-Curnamona克拉通；M-F-C-Madura-Forrest-Coompana省；MR-Miller Range；NC-Nornalup杂岩; TA-Terre Adélie克拉通; WAC-西澳克拉通；WI-Windmill群岛; WL-威尔克斯地

Figure 7. Tectonic map of Antarctica and Australia in a Gondwana configuration(modified after Liu et al., 2018)

AFO-Albany-Fraser Orogen; BH-Bunger Hills; CCr-Curnamona Craton; M-F-C-Madura-Forrest-Coompana Provinces; MR-Miller Range; NC-Nornalup Complex; TA-Terre Adélie Craton; WAC-West Australian Craton; WI-Windmill Islands; WL-Wilkes Land

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表 1 Bailey半岛镁铁质片麻岩和淡色片麻岩中锆石SHRIMP U-Pb同位素数据

Table 1. SHRIMP U-Pb isotopic analytical data of the mafic gneiss and leucogneiss from the Bailey Peninsula, Windmill Islands

点号	²⁰⁶Pb_c/%	含量/×10^-6			²³²Th/²³⁸U	年龄/Ma					同位素比值
点号	²⁰⁶Pb_c/%	U	Th	²⁰⁶Pb^*	²³²Th/²³⁸U	²⁰⁷Pb/²⁰⁶Pb	±1σ	²⁰⁶Pb/²³⁸U	±1σ	不和谐度	²⁰⁷Pb^/²⁰⁶Pb^	±/%	²⁰⁷Pb^*/²³⁵U	±/%	²⁰⁶Pb^*/²³⁸U	±/%	误差
C0121-1镁铁质片麻岩
1.1c	0.07	117	60	25.7	0.53	1406	35	1462	12	-4	0.0891	1.8	3.126	2.0	0.2545	0.91	0.4
2.1r	0.07	218	7	43.7	0.03	1322	27	1352	8	-2	0.0853	1.4	2.745	1.5	0.2334	0.7	0.4
3.1c	2.5	26	11	6.02	0.42	1224	200	1490	28	-22	0.0811	10.0	2.91	11.0	0.2601	2.1	0.2
4.1c	0.15	79	42	17.1	0.54	1439	44	1441	15	0	0.0906	2.3	3.13	2.6	0.2505	1.1	0.4
5.1r	0.04	1910	0	362	0.00	1328	9.1	1284	3	3	0.08556	0.47	2.599	0.55	0.22032	0.29	0.5
5.2r	1.35	127	1	27	0.01	1392	71	1406	12	-1	0.0884	3.7	2.97	3.8	0.2437	0.99	0.3
6.1c	0.29	118	47	24.8	0.41	1359	42	1406	12	-3	0.0869	2.2	2.922	2.4	0.2438	0.97	0.4
7.1c	0.27	92	30	20.1	0.34	1399	48	1458	14	-4	0.0888	2.5	3.107	2.7	0.2539	1.1	0.4
8.1c	0.0	70	38	15.8	0.56	1451	43	1497	23	-3	0.0912	2.3	3.288	2.9	0.2614	1.8	0.6
9.1c	0.1	108	39	23	0.37	1361	39	1431	13	-5	0.087	2.0	2.982	2.3	0.2486	1.0	0.5
10.1c	0.92	66	23	14.9	0.36	1500	77	1503	20	0	0.0936	4.1	3.39	4.3	0.2626	1.5	0.3
10.2r	0.08	200	5	40.9	0.03	1321	47	1375	10	-4	0.0853	2.4	2.795	2.6	0.2378	0.77	0.3
11.1c	0.34	80	24	17.3	0.31	1433	67	1440	15	0	0.0904	3.5	3.12	3.7	0.2503	1.2	0.3
12.1c	0.57	39	11	8.74	0.28	1389	69	1473	22	-6	0.0883	3.6	3.13	3.9	0.2567	1.7	0.4
13.1r	0.0	202	5	41.8	0.02	1324	27	1389	9	-5	0.0854	1.4	2.832	1.6	0.2405	0.73	0.5
14.1r	0.0	388	25	70.9	0.07	1205	22	1242	6	-3	0.08032	1.1	2.353	1.2	0.2125	0.55	0.4
15.1c	1.19	54	25	11.6	0.48	1343	130	1423	20	-6	0.0862	6.7	2.94	6.9	0.247	1.5	0.2
16.1c	0.29	108	32	22	0.31	1387	39	1374	18	1	0.0882	2.0	2.888	2.5	0.2375	1.5	0.6
17.1r	0.0	387	22	68.9	0.06	1239	22	1215	6	2	0.08173	1.1	2.338	1.3	0.2074	0.56	0.4
C0121-2淡色片麻岩
1.1r	0.02	1698	33	314	0.02	1196	11	1256	15	-5	0.07996	0.54	2.373	1.4	0.2152	1.3	0.9
2.1c	0.2	92	170	17.1	1.91	1191	50	1264	19	-6	0.0798	2.6	2.382	3.1	0.2166	1.7	0.6
3.1c	0.48	55	112	10.8	2.09	1335	62	1315	23	2	0.0859	3.2	2.68	3.7	0.2262	2.0	0.5
4.1r	0.02	2484	127	418	0.05	1229	11	1152	13	6	0.08132	0.56	2.195	1.4	0.1957	1.3	0.9
5.1c	0.82	106	125	18.2	1.22	1292	80	1166	19	10	0.084	4.1	2.29	4.5	0.1982	1.8	0.4
6.1r	0.04	3400	194	577	0.06	1247	10	1161	14	7	0.08207	0.53	2.233	1.4	0.1973	1.3	0.9
7.1c	0.69	153	411	26.7	2.78	1395	78	1186	18	15	0.0886	4.1	2.47	4.4	0.2021	1.7	0.4
8.1r	0.02	3436	233	576	0.07	1181	11	1149	13	3	0.07936	0.54	2.135	1.4	0.1951	1.3	0.9
9.1c	0.34	129	217	22.6	1.73	1240	45	1189	18	4	0.0818	2.3	2.285	2.8	0.2026	1.6	0.6
10.1c	0.28	150	183	26.7	1.26	1229	51	1213	27	1	0.0813	2.6	2.321	3.6	0.207	2.5	0.7
11.1r	0.09	2648	110	455	0.04	1277	11	1173	14	8	0.08331	0.56	2.293	1.4	0.1996	1.3	0.9
12.1c	0.51	506	305	87.7	0.62	1226	34	1179	15	4	0.0812	1.7	2.246	2.2	0.2006	1.4	0.6
13.1c	1.33	328	288	61.1	0.9	1337	59	1248	17	7	0.0859	3.1	2.53	3.4	0.2135	1.5	0.4
13.2r	0.08	2336	76	384	0.03	1180	14	1127	13	5	0.07932	0.7	2.089	1.5	0.191	1.3	0.9
14.1r	0.35	2191	73	366	0.03	1192	16	1142	14	4	0.07979	0.81	2.133	1.5	0.1939	1.3	0.8
注：误差为1s；Pb_c和Pb^*分别表示普通铅和放射成因铅；标准校正值的误差为1.03%；普通铅校正应用²⁰⁴Pb实测值；c: 锆石核(core)；r: 锆石增生边(rim)

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表 2 东南极Windmill群岛地质演化的锆石和独居石U-Pb年龄和石榴子石-全岩Sm-Nd同位素年龄记录

Table 2. Summary of litho-tectonic and metamorphic evolution as determined by U-Pb SHRIMP zircon and monazite analyses and Grt-WR Sm-Nd data

地质事件	样品地点及形式	年龄/Ma	分析方法	参考文献
Balaena岛辉长岩侵位		519	斜长石K-Ar	Webb et al., 1963
晚期粗玄岩墙侵位				Webb et al., 1963
细晶岩墙侵位	Robinson脊	1138±9	锆石SHRIMP U-Pb	Post，2000
变形作用(D₄)	北东-南西向左旋剪切和脆性断裂
橄榄石辉长岩墙侵位
变形作用(D₃)	早期构造单元的南北向褶皱
变形作用(D₂)	紧闭到等斜F2褶皱
Ardery紫苏花岗岩侵位	Bosner岛	1163±7	锆石SHRIMP U-Pb	Post，2000
	Robinson脊	1178±7, 1178±6	锆石LA-ICPMS U-Pb	Morrissey et al., 2017b
	Robinson脊	1196±8, 1205±13	锆石LA-ICPMS U-Pb	Zhang et al., 2012
Ford岛花岗岩侵位	Ford岛	1173±9	锆石SHRIMP U-Pb	Post，2000
黑云母花岗岩侵入变沉积岩	Mitchell半岛	1235±7	锆石LA-ICPMS U-Pb	Morrissey et al., 2017b
麻粒岩相和部分熔融和变形作用(M₂/D₂)	Mitchell半岛混合岩淡色体	1137±3	Sm-Nd(Grt-WR)	Post, 2000
	Herring岛麻粒岩变质事件	1142±7	独居石SHRIMP U-Pb	Post, 2000
	Bailey半岛正片麻岩	1156±17	Sm-Nd(Grt-WR)	Post, 2000
	Clark半岛正片麻岩	1169±7	独居石HRIMP U-Pb	Post, 2000
	Herring岛麻粒岩锆石变质增长边	1171±9	锆石SHRIMP U-Pb	Post, 2000
	Bailey半岛含正片麻岩	1171±13	独居石SHRIMP U-Pb	Post, 2000
	Clark半岛石榴黑云片麻岩淡色体	1171±6	独居石SHRIMP U-Pb	Post, 2000
	Cameron岛、Herring岛、Mitchell半岛和Robinson脊变沉积岩锆石变质边	ca.1325~1170	锆石LA-ICPMS U-Pb	Morrissey et al., 2017b
	Mitchell半岛、Herring岛变泥质岩	1177±4, 1200~1170，1185±8	独居石LA-ICPMS U-Pb	Morrissey et al., 2007a
	Bailey半岛正片麻岩同变质至变形后D_2a锆石变质增生	1214±10	锆石SHRIMP U-Pb	Post, 2000
	Bailey半岛淡色片麻岩锆石变质增生边	1197±26	锆石SHRIMP U-Pb	文中
	麻粒岩相重结晶	ca.1210~1180	锆石和独居石SHRIMP U-Pb，Sm-Nd(Grt-WR)	Post et al., 1997
花岗质岩石的侵位	Bailey含石榴子石花岗片麻岩侵位和片麻状含石榴子石花岗岩	1242±13, 1247±13, 1258±12	锆石LA-ICPMS U-Pb	Zhang et al., 2012
	Bailey半岛淡色片麻岩原岩侵位	1257±51	锆石SHRIMP U-Pb	文中
	Clark半岛正片麻岩	1315±6	锆石SHRIMP U-Pb	Post, 2000
	Clark半岛正片麻岩	1323±7	锆石LA-ICPMS U-Pb	Morrissey et al., 2017b
高角闪岩-麻粒岩相变质作用和变形作用(M₁/D₁)	角闪岩相重结晶	ca.1400~1300	锆石SHRIMP U-Pb	Post et al., 1997
	Mitchell半岛变泥质岩	1305±7	独居石LA-ICPMS U-Pb	Morrissey et al., 2007a
	Bailey半岛镁铁质片麻岩变质	1318±34	锆石SHRIMP U-Pb	文中
	Clark半岛石榴黑云片麻岩淡色体	1342±21	锆石SHRIMP U-Pb	Post, 2000
变沉积岩原岩沉积时代	Cameron岛、Herring岛、Mitchell半岛和Robinson脊变沉积岩	ca.1350~1315	锆石LA-ICPMS U-Pb	Morrissey et al., 2017b
	Herring岛石榴堇青黑云片麻岩	ca.1400~1350	锆石SHRIMP U-Pb	Post, 2000
	Chappel岛	1450±80	锆石SHRIMP U-Pb	Williams et al., 1983
		ca.2500~1700	锆石SHRIMP U-Pb	Post et al., 1997
花岗岩的侵位	Bailey半岛石榴花岗片麻岩、片麻状石榴花岗岩(继承锆石)	1372±13	锆石LA-ICPMS U-Pb	Zhang et al., 2012
镁铁质岩石的侵位	Bailey半岛	1403±28	锆石SHRIMP U-Pb	文中

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东南极Windmill群岛与罗迪尼亚超大陆聚合相关构造热事件的时代：来自Bailey半岛镁铁质片麻岩和淡色片麻岩锆石SHRIMP U-Pb年龄的约束

doi: 10.12090/j.issn.1006-6616.2021.27.05.063

作者简介:
王彦斌(1966-), 男, 博士, 研究员, 从事同位素地质年代学和地球化学研究工作。E-mail: wangyanbin@bjshrimp.cn

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Zircon U-Pb ages of the mafic gneiss and leucogneiss from the Bailey Peninsula: Constraints on the timing of the tectonothermal events related to the amalgamation of Rodinia in the Windmill Islands, East Antarctica

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东南极Windmill群岛与罗迪尼亚超大陆聚合相关构造热事件的时代：来自Bailey半岛镁铁质片麻岩和淡色片麻岩锆石SHRIMP U-Pb年龄的约束

doi: 10.12090/j.issn.1006-6616.2021.27.05.063

作者简介: 王彦斌(1966-), 男, 博士, 研究员, 从事同位素地质年代学和地球化学研究工作。E-mail: wangyanbin@bjshrimp.cn

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Zircon U-Pb ages of the mafic gneiss and leucogneiss from the Bailey Peninsula: Constraints on the timing of the tectonothermal events related to the amalgamation of Rodinia in the Windmill Islands, East Antarctica

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作者简介:
王彦斌(1966-), 男, 博士, 研究员, 从事同位素地质年代学和地球化学研究工作。E-mail: wangyanbin@bjshrimp.cn