西拉木伦河缝合带北侧二叠纪砂岩碎屑锆石

韩国卿; 刘永江; 温泉波; 李伟; 吴琳娜; 赵英利; 丁凌; 赵立敏; 梁琛岳

doi:10.3799/dqkx.2011.070

西拉木伦河缝合带北侧二叠纪砂岩碎屑锆石

doi: 10.3799/dqkx.2011.070

韩国卿^{1, 2,},
刘永江^1, ,,
温泉波¹,
李伟¹,
吴琳娜^{1, 3},
赵英利¹,
丁凌^{1, 4},
赵立敏¹,
梁琛岳¹

1.
吉林大学地球科学学院，吉林长春 130061
2.
萨尔茨堡大学地质与地理系，奥地利萨尔茨堡 A-5020
3.
冀东油田勘探开发研究院，河北唐山 063004
4.
中国冶金地质总局第一地质勘查院，河北燕郊 101601

基金项目:

国家自然科学重点基金项目 40739905

博士点基金项目 200801830041

国家油气专项 2009GYXQ12

中国石油化工股份有限公司科技开发项目 G0800-06-ZS-327

国家留学基金建设高水平大学公派研究生项目 2008617114

详细信息

作者简介:
韩国卿(1982-)，男，博士研究生，主要从事构造地质学和构造年代学研究.E-mail: hanguoqingster@yahoo.cn

通讯作者:
刘永江，E-mail: yongjiang@jlu.edu.cn

中图分类号: P597
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出版历程
- 收稿日期: 2010-11-16
- 刊出日期: 2011-07-01

LA-ICP-MS U-Pb Dating of Detrital Zircons from the Permian Sandstones in North Side of Xar Moron River Suture Belt and Its Tectonic Implications

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Institute of Geology and Palaeontology, University of Salzburg, Salzburg A-5020, Austria
3.
Research Institute of Exploration and Development, Jidong Oilfield, Tangshan 063004, China
4.
The 1st Geological Exploration Institute of China Exploration Bureau, Yanjiao 101601, China

摘要

摘要: 研究区位于西拉木伦河缝合带北侧，地理位置位于内蒙古东部草原区、大兴安岭南段，构造部位介于苏尼特左旗-锡林浩特-西乌珠穆沁旗南缝合线和西拉木伦河缝合带之间，是讨论华北地块北缘与其北侧地块拼贴过程的关键地区.通过对西拉木伦河缝合带北侧克什克腾旗(简称克旗)和林西地区二叠纪砂岩进行碎屑锆石LA-ICP-MS U-Pb年代学研究，认为克旗地区原中二叠世“哲斯组”可能为一套晚二叠世甚至早三叠世沉积.克旗、林西地区二叠纪的沉积物源主要来自其北侧的苏尼特左旗-锡林浩特-西乌旗南的岩浆弧，并有华北板块北缘物源混入，华北板块北缘与其北侧地块应在晚二叠世林西组沉积时期已经开始碰撞，导致林西地区林西组沉积具有南北两侧混合物源特征，板块碰撞的最终闭合的时间应在250 Ma左右.
- 缝合带 /
- 砂岩 /
- 锆石 /
- 地质年代学 /
- 构造学
Abstract: The study area is geographically located in the northern side of Xar Moron River suture belt in the eastern Inner Mongolia and the southern Da Hingg'an Mountains and tectonically between the Sonidzuoqi-Xilinhot-southern Xi Ujimqin suture belt and Xar Moron River suture belt. It's a key area for the study on the collision process between the northern margin of North China Plate and the blocks to the north. The detrital zircons from Permian sandstones in Hexigten Banner (Keqi for short) and Linxi areas in the northern side of Xar Moron River suture belt have been dated by LA-ICP-MS U-Pb method. The dating results suggest that the previous Mid-Permian "Zhesi" Fm. is probably a Late Permian or even Early Triassic sedimentary sequence. The provenance of the Permian sediments in Keqi and Linxi areas is mainly from Sonidzuoqi-Xilinhot-sourthern Xi Ujimqin magma arc in the north, and partly from the northern margin of North China Plate. It is indicated that the collision between the northern margin of North China Plate and the blocks to the north had started in Late Permian during the Linxi Fm. depositing, the Permian sediments' provenance in Linxi and Keqi areas mixed those from the north and south, and the final closure time was about 250 Ma.
- suture belt /
- sandstones /
- zircons /
- geochronology /
- tectonics

HTML全文

图 1 研究区大地构造背景(据Jian et al., 2008, 修改)

Fig. 1. Sketch map of the geology of research field

下载: 全尺寸图片幻灯片

图 2 克旗和林西地区

1.下元古界宝音图群；2.中二叠统哲斯组；3.下泥盆统西别河组；4.中二叠统于家北沟组；5.石炭系辉长岩；6.上二叠统林西组；7.上石炭统本巴图组；8.二叠纪花岗岩组合；9.下二叠统大石寨组；10.三叠纪花岗岩；11.下二叠统额里图组；12.后三叠纪地层；13.水体；14.缝合带；15.张性断裂；16.压性断裂；17.性质不明断裂；18.推测断裂；19.采样位置点

Fig. 2. Geology map of Linxi and Keqi areas

下载: 全尺寸图片幻灯片

图 3 锆石CL图像

a.克旗地区；b.林西地区

Fig. 3. CL images of selected zircons from Permian sandstones

下载: 全尺寸图片幻灯片

图 4 碎屑锆石U-Pb谐和图

a.克旗地区；b.林西地区

Fig. 4. Concordia plots of zircons from Permian sandstones

下载: 全尺寸图片幻灯片

图 5 锆石年龄频率分布

a，b为克旗地区；c，d为林西地区；e，f为苏尼特左旗岩浆岩和锡林浩特杂岩；右图是左图的局部放大；数据来源于Chen et al., 2000, 2009; 陈斌等，2001；Shi et al., 2003；石玉若等, 2004, 2005a, b，2007

Fig. 5. Correlation to probability diagram of zircon ages for the Permian sandstones

下载: 全尺寸图片幻灯片

表 1 克旗和林西地区二叠系地层(据邵济安等, 2007, 略有修改)

Table 1. The Permian strata in Keqi and Linxi areas

地层时代	组	岩性特征及上下地层间关系
P₃	林西组	分布广泛，岩性较单一，主要由黑色板岩、粉砂质板岩、粉砂岩、砂岩组成，含植物和淡水双壳类化石，上限不清，下部与早二叠统为整合或平行不整合接触关系，出露厚度一般为2 699 m；在区域上由若干沉积盆地组成，横向上各盆地由西向东碎屑岩粒度变细，纵向上由下向上碎屑粒度变细；该组湖相和深湖相沉积所含动、植物化石的时代为晚二叠世，植物化石为安哥拉植物群
P₂	哲斯组	原称黄岗梁组、西乌旗组，下部为黄绿色砂砾岩、灰色生物碎屑岩和硅质岩，含大量早二叠世中晚期的腕足类、珊瑚和少量苔藓虫，不含GFDA2；上部为灰色块状炭质粉砂岩、板岩，夹灰岩透镜体，海相化石以腕足类为主，菊石等次之，并有大量植物化石，总厚2 238 m；其上与林西组连续沉积，其下与大石寨组为角度不整合关系
P₁	大石寨组	分布广泛，为浅海-滨海相的细碧岩、角斑岩及凝灰岩组合，夹正常碎屑岩，含早二叠世早期的腕足、珊瑚、苔藓等化石，厚2 680 m；该组地层呈北东向展布，可分为北(西乌旗经罕乌拉到霍林河市南都)、中(哈尔呼舒到大石寨)、南(巴林右旗到科尔沁右翼中旗)3个带；底部为一套滨海相砂、板岩组合，下限不清，部分学者称其为青风山组.在巴林左旗碧流台、科尔沁右翼中旗等地该碎屑岩出露较好

下载: 导出CSV

表 2 克旗、林西地区二叠纪砂岩碎屑锆石U-Pb同位素数据(*号表示²⁰⁶Pb/²³⁸U相对于²⁰⁷Pb/²⁰⁶Pb偏差大于或小于10%的锆石颗粒)

Table 2. Results of LA-ICP-MS zircon U-Pb age dating for the Permian sandstones from Keqi and Linxi areas

分析点号	组成(mg·g^-1)			Th/U	同位素比值						年龄(Ma)
分析点号	Pb	Th	U	Th/U	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ
212KQ-1-01^*	40	44	266	0.17	0.067 2	0.001 8	1.254 2	0.029 0	0.135 4	0.001 6	843	55	825	13	819	9
212KQ-1-02^*	4	42	70	0.61	0.065 7	0.004 0	0.396 3	0.023 2	0.043 8	0.000 7	795	131	339	17	276	4
212KQ-1-03	103	193	268	0.72	0.119 5	0.001 7	5.386 4	0.081 0	0.327 7	0.003 8	1 949	13	1 883	13	1 827	18
212KQ-1-04	78	473	705	0.67	0.061 4	0.000 9	0.769 7	0.011 9	0.091 2	0.001 0	653	16	580	7	562	6
212KQ-1-05	77	311	465	0.67	0.076 9	0.001 3	1.440 9	0.024 8	0.136 2	0.001 6	1 119	17	906	10	823	9
212KQ-1-06	26	227	353	0.64	0.065 3	0.002 2	0.459 0	0.014 4	0.051 0	0.000 6	784	73	384	10	321	4
212KQ-1-07	20	212	360	0.59	0.057 2	0.002 0	0.355 5	0.012 4	0.045 2	0.000 6	498	53	309	9	285	4
212KQ-1-08	31	420	535	0.79	0.058 8	0.001 8	0.347 4	0.010 3	0.043 0	0.000 6	559	42	303	8	271	3
212KQ-1-09	71	171	336	0.51	0.070 8	0.001 1	1.393 9	0.022 9	0.143 1	0.001 7	951	16	886	10	862	9
212KQ-1-10	8	15	32	0.47	0.084 0	0.002 1	2.478 8	0.060 8	0.214 5	0.002 8	1 291	28	1 266	18	1 253	15
212KQ-1-11	3	67	54	1.24	0.052 0	0.003 2	0.296 9	0.017 6	0.041 5	0.000 7	285	104	264	14	262	5
212KQ-1-12	18	154	363	0.42	0.055 6	0.001 1	0.316 0	0.006 4	0.041 3	0.000 5	437	25	279	5	261	3
212KQ-1-13	83	50	516	0.10	0.070 5	0.001 4	1.471 9	0.023 5	0.151 4	0.001 7	943	41	919	10	909	10
212KQ-1-14	21	275	373	0.74	0.055 1	0.001 0	0.315 3	0.005 9	0.041 5	0.000 5	417	22	278	5	262	3
212KQ-1-15	12	123	217	0.57	0.055 9	0.002 0	0.329 0	0.011 4	0.042 7	0.000 6	448	52	289	9	270	4
212KQ-1-16	25	383	453	0.84	0.055 7	0.001 5	0.332 0	0.008 8	0.043 3	0.000 6	440	36	291	7	273	3
212KQ-1-17	11	64	207	0.31	0.054 5	0.001 8	0.372 5	0.011 7	0.049 6	0.000 6	390	78	321	9	312	4
212KQ-1-18	12	195	224	0.87	0.056 1	0.001 5	0.317 4	0.008 3	0.041 1	0.000 5	456	36	280	6	259	3
212KQ-1-19	11	108	214	0.51	0.056 6	0.001 7	0.315 2	0.009 2	0.040 4	0.000 5	476	41	278	7	255	3
212KQ-1-20	18	157	327	0.48	0.052 2	0.001 1	0.333 0	0.007 0	0.046 3	0.000 6	292	26	292	5	292	3
212KQ-1-21	7	143	136	1.05	0.053 8	0.001 3	0.305 8	0.007 3	0.041 2	0.000 5	363	32	271	6	260	3
212KQ-1-22^*	18	51	97	0.52	0.063 3	0.003 8	0.708 4	0.041 7	0.081 2	0.001 5	718	93	544	25	503	9
212KQ-1-23	21	223	418	0.53	0.054 7	0.001 1	0.321 0	0.006 3	0.042 6	0.000 5	399	24	283	5	269	3
212KQ-1-24	22	620	311	1.99	0.054 9	0.001 1	0.328 5	0.006 8	0.043 4	0.000 5	406	25	288	5	274	3
212KQ-1-25	13	116	206	0.56	0.055 5	0.002 3	0.410 7	0.016 1	0.053 7	0.000 7	430	94	349	12	337	4
212KQ-1-26	52	52	343	0.15	0.066 5	0.001 6	1.246 2	0.025 3	0.135 9	0.001 6	822	50	822	11	822	9
212KQ-1-27	76	116	261	0.44	0.146 6	0.003 5	5.444 5	0.111 0	0.269 3	0.003 4	2 307	42	1 892	17	1 537	17
212KQ-1-28	5	42	69	0.61	0.055 1	0.003 8	0.350 0	0.023 6	0.046 1	0.000 8	416	160	305	18	290	5
212KQ-1-29	24	291	425	0.68	0.051 7	0.002 4	0.300 9	0.013 2	0.042 3	0.000 6	270	108	267	10	267	3
212KQ-1-30	24	290	456	0.64	0.053 2	0.001 0	0.321 4	0.006 4	0.043 8	0.000 5	339	24	283	5	276	3
212KQ-1-31	70	137	330	0.41	0.076 6	0.001 2	2.104 5	0.034 6	0.199 1	0.002 4	1 111	16	1 150	11	1 170	13
212KQ-1-32	8	108	161	0.67	0.057 3	0.001 7	0.354 3	0.010 2	0.044 8	0.000 6	503	40	308	8	283	4
212KQ-1-33	107	197	501	0.39	0.079 1	0.001 2	2.160 7	0.035 1	0.198 0	0.002 4	1 175	15	1 168	11	1 164	13
212KQ-1-34	18	187	320	0.59	0.054 7	0.001 2	0.376 0	0.008 3	0.049 8	0.000 6	400	27	324	6	313	4
212KQ-1-35	26	400	446	0.90	0.053 5	0.001 1	0.333 5	0.006 7	0.045 1	0.000 6	352	24	292	5	285	3
212KQ-1-36	25	190	503	0.38	0.055 1	0.001 0	0.328 6	0.006 4	0.043 2	0.000 5	418	23	289	5	273	3
212KQ-1-37	11	168	181	0.93	0.057 0	0.001 5	0.346 1	0.009 4	0.044 0	0.000 6	493	37	302	7	277	4
212KQ-1-38	19	101	198	0.51	0.056 6	0.001 4	0.601 3	0.015 2	0.077 0	0.001 0	476	33	478	10	478	6
212KQ-1-39	6	58	109	0.53	0.048 9	0.001 8	0.346 1	0.012 6	0.051 3	0.000 7	143	59	302	10	322	4
212KQ-1-40	44	150	232	0.65	0.072 0	0.001 3	1.624 8	0.029 5	0.163 5	0.002 0	986	18	980	11	976	11
212KQ-1-41	6	21	59	0.36	0.056 8	0.002 1	0.650 9	0.022 0	0.083 1	0.001 1	483	82	509	14	515	6
212KQ-1-42^*	88	189	409	0.46	0.077 8	0.001 4	2.095 4	0.038 3	0.195 3	0.002 4	1 140	18	1 147	13	1 150	13
212KQ-1-43	25	358	417	0.86	0.055 4	0.001 4	0.389 8	0.009 9	0.051 0	0.000 7	430	34	334	7	320	4
212KQ-1-44	10	130	164	0.79	0.058 3	0.001 6	0.395 0	0.010 8	0.049 1	0.000 7	540	37	338	8	309	4
212KQ-1-45	18	107	221	0.48	0.053 6	0.002 7	0.419 1	0.020 3	0.056 7	0.000 8	355	117	355	15	355	5
212KQ-1-46	9	93	172	0.54	0.052 2	0.002 3	0.283 3	0.012 0	0.039 4	0.000 6	294	105	253	10	249	3
212KQ-1-47	4	73	62	1.18	0.068 9	0.003 5	0.337 4	0.016 1	0.035 5	0.000 8	895	63	295	12	225	5
212KQ-1-48	6	82	109	0.75	0.053 2	0.001 7	0.291 1	0.009 2	0.039 6	0.000 6	339	46	259	7	250	3
212KQ-1-49	26	295	485	0.61	0.055 0	0.001 2	0.372 8	0.008 5	0.049 1	0.000 6	411	28	322	6	309	4
212KQ-1-50	24	242	462	0.52	0.057 2	0.001 1	0.356 8	0.007 2	0.045 2	0.000 6	500	23	310	5	285	4
212KQ-1-51	53	68	164	0.41	0.091 4	0.001 7	3.443 4	0.065 7	0.273 1	0.003 5	1 454	18	1 514	15	1 557	18
212KQ-1-52	11	143	153	0.93	0.057 4	0.002 3	0.358 7	0.014 2	0.045 3	0.000 7	506	61	311	11	286	4
212KQ-1-53	14	116	275	0.42	0.055 8	0.001 5	0.352 8	0.009 6	0.045 8	0.000 6	445	37	307	7	289	4
212KQ-1-54	18	249	286	0.87	0.052 0	0.003 2	0.289 9	0.017 5	0.040 5	0.000 6	284	144	259	14	256	4
212KQ-1-55	73	273	406	0.67	0.069 9	0.001 2	1.499 5	0.028 4	0.155 4	0.002 0	926	19	930	12	931	11
212KQ-1-56	11	177	227	0.78	0.048 8	0.001 6	0.265 0	0.008 8	0.039 4	0.000 6	137	52	239	7	249	3
212KQ-1-57	53	98	386	0.25	0.059 5	0.001 1	0.908 4	0.018 1	0.110 7	0.001 4	584	22	656	10	677	8
212KQ-1-58	11	122	225	0.54	0.055 4	0.001 2	0.330 2	0.007 3	0.043 2	0.000 6	428	27	290	6	273	4
212KQ-1-59	54	59	177	0.33	0.093 7	0.001 7	3.479 8	0.067 4	0.269 1	0.003 5	1 503	18	1 523	15	1 536	18
212KQ-1-60	20	105	115	0.91	0.065 2	0.004 6	0.787 0	0.053 3	0.087 6	0.001 5	781	151	589	30	541	9
227LX-1-01	108	112	217	0.52	0.137 3	0.001 7	7.644 4	0.101 4	0.403 6	0.004 6	2 194	10	2 190	12	2 186	21
227LX-1-02	231	177	471	0.38	0.132 9	0.001 7	7.283 4	0.095 8	0.397 4	0.004 5	2 137	10	2 147	12	2 157	21
227LX-1-03	39	156	344	0.45	0.058 6	0.001 6	0.738 4	0.018 7	0.091 5	0.001 1	550	62	561	11	564	6
227LX-1-04	37	81	47	1.73	0.165 0	0.002 2	10.744 8	0.150 6	0.472 2	0.005 5	2 507	11	2 501	13	2 493	24
227LX-1-05	96	65	238	0.27	0.117 9	0.001 5	5.525 8	0.074 3	0.339 9	0.003 9	1 924	11	1 905	12	1 886	19
227LX-1-06	21	168	234	0.72	0.056 7	0.000 9	0.551 5	0.008 8	0.070 5	0.000 8	479	17	446	6	439	5
227LX-1-07	22	165	248	0.67	0.056 0	0.000 9	0.559 9	0.009 2	0.072 5	0.000 8	454	18	451	6	451	5
227LX-1-08	12	179	191	0.94	0.052 2	0.002 6	0.329 9	0.016 0	0.045 8	0.000 6	294	117	289	12	289	4
227LX-1-09	116	141	330	0.43	0.058 6	0.001 0	0.609 7	0.010 8	0.075 5	0.000 9	552	20	483	7	469	5
227LX-1-10	44	27	385	0.07	0.060 9	0.001 3	0.865 6	0.015 0	0.103 1	0.001 2	635	46	633	8	633	7
227LX-1-11	57	84	136	0.62	0.111 5	0.002 7	5.061 5	0.108 0	0.329 3	0.004 0	1 823	46	1 830	18	1 835	19
227LX-1-12	333	51	860	0.06	0.116 2	0.001 5	5.495 0	0.073 6	0.342 9	0.003 9	1 899	11	1 900	12	1 901	19
227LX-1-13	23	33	52	0.63	0.117 1	0.001 7	5.533 1	0.083 5	0.342 5	0.004 0	1913	13	1906	13	1899	19
227LX-1-14^*	14	141	197	0.71	0.099 2	0.001 7	0.659 2	0.011 3	0.048 2	0.000 6	1 608	16	514	7	304	4
227LX-1-15	126	73	301	0.24	0.120 7	0.001 6	5.958 2	0.081 5	0.357 9	0.004 1	1 967	11	1 970	12	1 972	19
227LX-1-16	25	148	289	0.51	0.056 5	0.001 7	0.553 9	0.015 7	0.071 2	0.000 9	470	70	448	10	443	5
227LX-1-17	18	109	203	0.54	0.056 6	0.000 9	0.600 3	0.010 2	0.076 9	0.000 9	476	19	477	6	478	5
227LX-1-18	146	60	402	0.15	0.107 9	0.001 4	4.678 5	0.065 2	0.314 6	0.003 6	1 763	12	1 763	12	1 763	18
227LX-1-19	298	47	672	0.07	0.122 0	0.001 6	6.078 1	0.084 6	0.361 2	0.004 1	1 986	11	1 987	12	1 988	20
227LX-1-20^*	6	52	89	0.59	0.060 9	0.002 5	0.464 1	0.018 4	0.055 3	0.000 8	636	59	387	13	347	5
227LX-1-21	107	118	264	0.45	0.119 7	0.001 7	5.831 0	0.085 4	0.353 2	0.004 1	1 952	12	1 951	13	1 950	19
227LX-1-22	66	75	162	0.47	0.114 6	0.001 6	5.316 9	0.076 6	0.336 5	0.003 9	1 873	12	1 872	12	1 870	19
227LX-1-23	30	147	362	0.41	0.055 1	0.000 9	0.553 6	0.009 3	0.072 9	0.000 9	416	19	447	6	453	5
227LX-1-24	62	63	97	0.65	0.169 9	0.002 4	11.343 7	0.169 5	0.484 3	0.005 7	2 556	12	2 552	14	2 546	25
227LX-1-25	59	216	650	0.33	0.057 1	0.000 9	0.623 1	0.009 6	0.079 2	0.000 9	493	16	492	6	491	5
227LX-1-26	20	73	243	0.30	0.056 7	0.001 0	0.599 1	0.010 4	0.076 6	0.000 9	481	19	477	7	476	5
227LX-1-27	6	61	115	0.53	0.052 6	0.002 5	0.319 1	0.014 8	0.044 0	0.000 6	312	112	281	11	278	4
227LX-1-28	22	110	248	0.45	0.057 1	0.001 3	0.587 7	0.013 4	0.074 6	0.000 9	495	29	469	9	464	6
227LX-1-29	126	183	271	0.67	0.116 9	0.001 6	5.555 4	0.081 6	0.344 7	0.004 0	1 909	12	1 909	13	1 909	19
227LX-1-30	78	114	868	0.13	0.056 7	0.000 9	0.651 4	0.010 1	0.083 3	0.001 0	481	16	509	6	516	6
227LX-1-31	15	142	267	0.53	0.052 8	0.001 0	0.370 3	0.007 2	0.050 9	0.000 6	318	24	320	5	320	4
227LX-1-32	12	82	138	0.59	0.056 0	0.001 1	0.561 1	0.011 0	0.072 7	0.000 9	452	23	452	7	452	5
227LX-1-33	35	234	415	0.56	0.056 2	0.000 9	0.559 3	0.009 2	0.072 2	0.000 8	460	18	451	6	449	5
227LX-1-34	159	41	415	0.10	0.115 9	0.001 7	5.461 8	0.082 6	0.341 6	0.004 0	1 895	13	1 895	13	1 895	19
227LX-1-35	82	149	182	0.82	0.116 7	0.001 8	5.532 1	0.086 4	0.343 9	0.004 0	1 906	13	1 906	13	1 905	19
227LX-1-36	25	448	373	1.20	0.052 5	0.000 9	0.353 9	0.006 3	0.048 9	0.000 6	305	21	308	5	308	4
227LX-1-37	14	25	37	0.69	0.107 0	0.001 8	4.587 6	0.079 7	0.310 9	0.003 7	1 749	16	1 747	14	1 745	18
227LX-1-38	18	137	219	0.63	0.058 8	0.001 0	0.574 5	0.010 3	0.070 9	0.000 8	559	20	461	7	442	5
227LX-1-39	125	160	481	0.33	0.076 6	0.001 2	2.001 8	0.032 6	0.189 5	0.002 2	1 111	16	1 116	11	1 119	12
227LX-1-40	11	73	130	0.56	0.056 3	0.001 3	0.587 3	0.013 2	0.075 6	0.000 9	465	29	469	8	470	6
227LX-1-41	44	96	95	1.01	0.112 0	0.001 9	5.121 9	0.090 8	0.331 6	0.004 0	1 833	16	1 840	15	1 846	19
227LX-1-42	188	99	313	0.32	0.168 0	0.002 6	11.191 6	0.182 0	0.483 1	0.005 7	2 538	13	2 539	15	2 541	25
227LX-1-43	12	89	131	0.68	0.062 8	0.001 5	0.671 3	0.016 1	0.077 6	0.001 0	700	30	521	10	482	6
227LX-1-44	107	67	322	0.21	0.105 9	0.001 7	4.431 5	0.072 7	0.303 5	0.003 6	1 730	15	1 718	14	1 709	18
227LX-1-45	27	271	491	0.55	0.059 4	0.001 0	0.387 7	0.006 9	0.047 4	0.000 6	581	20	333	5	298	3
227LX-1-46	22	199	251	0.80	0.057 1	0.001 1	0.579 2	0.011 2	0.073 6	0.000 9	496	23	464	7	458	5
227LX-1-47	83	69	147	0.47	0.153 5	0.002 5	9.489 3	0.160 4	0.448 3	0.005 3	2 386	14	2 387	16	2 387	24
227LX-1-48	58	87	132	0.66	0.113 7	0.002 0	5.240 1	0.092 8	0.334 4	0.004 0	1 859	16	1 859	15	1 859	19
227LX-1-49	84	40	225	0.18	0.115 2	0.001 9	5.420 4	0.092 1	0.341 2	0.004 0	1 883	15	1 888	15	1 893	19
227LX-1-50	102	68	167	0.41	0.159 7	0.002 7	10.217 8	0.175 1	0.464 0	0.005 5	2 452	14	2 455	16	2 457	24
227LX-1-51	159	125	247	0.50	0.164 2	0.002 8	10.683 3	0.185 1	0.471 8	0.005 6	2 500	14	2 496	16	2 491	25
227LX-1-52	16	7	184	0.04	0.059 6	0.001 4	0.703 7	0.014 4	0.085 7	0.001 0	588	53	541	9	530	6
227LX-1-53	11	73	120	0.60	0.058 1	0.002 6	0.614 4	0.026 2	0.076 7	0.001 0	534	100	486	17	476	6
227LX-1-54	9	40	105	0.38	0.059 7	0.001 3	0.645 9	0.014 4	0.078 5	0.001 0	592	27	506	9	487	6
227LX-1-55	119	123	199	0.62	0.166 8	0.002 9	11.003 5	0.193 7	0.478 6	0.005 7	2 525	15	2 523	16	2 521	25
227LX-1-56	95	109	238	0.46	0.117 1	0.002 0	5.551 7	0.099 4	0.343 8	0.004 1	1 913	16	1 909	15	1 905	20
227LX-1-57	46	51	113	0.45	0.115 0	0.002 1	5.349 3	0.099 7	0.337 5	0.004 1	1 879	17	1 877	16	1 875	20
227LX-1-58	71	77	421	0.18	0.074 1	0.002 0	1.527 1	0.037 7	0.149 4	0.001 8	1 045	57	941	15	897	10
227LX-1-59	18	152	335	0.45	0.056 0	0.001 2	0.387 1	0.008 6	0.050 2	0.000 6	451	28	332	6	316	4
227LX-1-60	30	54	616	0.09	0.053 0	0.001 1	0.355 6	0.007 4	0.048 7	0.000 6	328	26	309	6	306	4
注：标星号“*”的样品数据为不和谐的数据点.

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参考文献(114)

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