海拉尔盆地早白垩世早期挤压变形事件的厘定及其构造意义

张科峰; 邓彬; 章凤奇; 阿敏娜; 陈汉林; 杨树锋; 蒙启安; 梁江平; 王卓卓

doi:10.3799/dqkx.2016.094

海拉尔盆地早白垩世早期挤压变形事件的厘定及其构造意义

doi: 10.3799/dqkx.2016.094

张科峰^1,2,,
邓彬^1,2,
章凤奇^1,2,3, ,,
阿敏娜^1,2,
陈汉林^1,2,
杨树锋^1,2,
蒙启安⁴,
梁江平⁴,
王卓卓⁴

1.
浙江大学地球科学学院，浙江杭州 310027
2.
教育部含油气盆地构造研究中心，浙江杭州 310027
3.
西澳大学地球与环境学院，澳大利亚珀斯 WA 6009
4.
大庆油田勘探开发研究院，黑龙江大庆 163712

基金项目:

中央高校基本科研业务费专项资金资助项目 2016QNA3013

国家重大科技专项课题 2011ZX05009-001

国家自然科学基金项目 41330207

国家自然科学基金项目 41272231

详细信息

作者简介:
张科峰(1989-)，男，博士，主要从事构造地质学方面研究.E-mail：765280910@qq.com

通讯作者:
章凤奇, E-mail：zhangfq78@zju.edu.cn

中图分类号: P542
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- 被引次数: 0
出版历程
- 收稿日期: 2015-07-30
- 刊出日期: 2016-07-15

Determination of Early Stage of Early Cretaceous Compressive Event in Hailar Basin, NE China, and Its Tectonic Significance

Zhang Kefeng^{1,2
,},
Deng Bin^1,2,
Zhang Fengqi^{1,2,3
, ,},
A Minna^1,2,
Chen Hanlin^1,2,
Yang Shufeng^1,2,
Meng Qi'an⁴,
Liang Jiangping⁴,
Wang Zhuozhuo⁴

1.
School of Earth Sciences, Zhejiang University, Hangzhou 310027, China
2.
Structural Research Center of Oil & Gas Bearing Basin, Ministry of Education, Hangzhou 310027, China
3.
School of Earth and Environment, The University of Western Australia, Perth, WA6009, Australia
4.
Research Institute of Petroleum Exploration and Development, Daqing Oil eld Co. Ltd., Daqing 163712, China

摘要

摘要: 中生代发生在东北亚地区的蒙古-鄂霍次克造山作用一直是国内外地学界十分关注的大地构造事件.综合利用油气勘探新获取的地震反射、钻井、测井等资料，在海拉尔盆地贝尔凹陷早白垩世断陷层序之下识别出一套卷入强烈挤压变形的构造层.构造解析表明它主要由一条北东东向的逆掩断层及其相关的冲断-褶皱变形系统构成.地层岩性特征和碎屑锆石U-Pb测年结果显示，这是一套沉积于晚侏罗世末期的陆相湖盆碎屑岩建造，区域上应归属上侏罗统塔木兰沟组；结合上覆早白垩世断陷盆地的发育和邻区同期变质核杂岩体隆升剥露时代，提出海拉尔盆地这期冲断-褶皱变形事件发生在早白垩世早期(ca. 145~133 Ma)，是晚中生代蒙古-鄂霍次克洋闭合后进入强烈陆内造山作用的构造变形记录.
- 海拉尔盆地 /
- 挤压事件 /
- 碎屑锆石U-Pb定年 /
- 蒙古-鄂霍次克造山作用 /
- 早白垩世早期 /
- 地质年代学 /
- 构造地质
Abstract: The Mesozoic Mongol-Okhotsk orogeny in Northeast Asia is a significant tectonic event which has attracted interest of many geologists. A tectonic unit involved in strong contractional deformation has been identified under the Early Cretaceous rifting sequences in the Beier depression of the Hailar basin, based on the newly obtained petroleum exploration data including seismic reflection, drilling and well logging. Structural analyses show that the structural system is composed of one major ENE trending overthrust fault and associated thrusting-folding deformations. Lithological and stratigraphic characteristics and dating results of detrital zircon U-Pb show that the strata consist of Late Jurassic terrigenous clastic rock, as a part of the Upper Jurassic Tamulangou Formation in this region. Considering the time of the development of overlying faulted basins and the emplacement of coeval metamorphic core complexes in surrounding area, it is suggested that the thrusting-folding event of the Hailar basin mainly occurred during early stage of the Early Cretaceous (145-133 Ma), which is a key structural record resulted from the Mongol-Okhotsk collisional orogeny during the Late Mesozoic.
- Hailar basin /
- compressive event /
- detrital zircon U-Pb dating /
- Mongol-Okhotsk orogeny /
- early stage of Early Cretaceous /
- geochronology /
- tectonic geology

HTML全文

图 1 中国东北及邻区晚中生代裂陷盆地群分布(a)、海拉尔-塔木察格盆地内部凸起与凹陷等构造单元分布(灰色区域为凹陷)(b)和贝尔凹陷早白垩世早期挤压构造与早白垩世中晚期控陷正断层格架(c)

EG.东戈壁盆地；EL.二连盆地；HL.海拉尔盆地；SL.松辽盆地；YG.银根盆地.BR.贝尔凹陷

Fig. 1. Distribution of the Late Mesozoic rift basins in NE China and adjacent areas (a), inner uplift and depressions (grey area in colour are depressions) in the Hailar-Tamsag basin (b) and sketch of early stage of Early Cretaceous compressive structures and middle-late stage of Early Cretaceous main normal faults in the Beier depression (c)

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图 2 海拉尔盆地地层柱状图

据A et al.(2013)修改

Fig. 2. Stratigraphic chart for the Hailar basin

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图 3 海拉尔盆地贝尔凹陷东南部地震解释剖面与对应的原始地震剖面

T₆, T₅, T₃, T_2-2, T₂和T₀₄地震反射层所对应的地层界面见图 2；剖面位置见图 1c；1.上白垩统；2.下白垩统；3.上侏罗统；4.正断层；5.逆冲断层.J₃t.塔木兰沟组；K₁t.铜钵庙组；K₁n.南屯组；K₁d.大磨拐河组；K₁y.伊敏组；K₂q.青元冈组

Fig. 3. Seismic interpretation and their original seismic profiles in the southeastern Beier depression, Hailar basin

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图 4 海拉尔盆地贝尔凹陷贝48井晚侏罗世碎屑岩层序的典型岩心照片

a.灰色泥质粉砂岩，深度1 118.67 m；b.灰色长石砂岩，深度1 121.99 m；c.灰色粉沙质泥岩与灰白色钙质泥岩薄互层，1 149.24 m；d.灰白色长石中砂岩，底部可见典型河道冲刷面和底部滞留钙质泥砾，深度1 252.39~1 152.69 m；e.深灰色长石岩屑粗砂岩，发育典型槽状交错层理，深度1 484.48~1 484.66 m；f.灰色含黑色炭屑粉砂岩，深度1 487.68 m；g.紫红色、青灰色致密块状中-细砂岩，深度3 081.73~3 082.33 m

Fig. 4. Photos of typical cores of Upper Jurassic clastic rocks from well Bei 48 in Beier depression, Hailar basin

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图 5 海拉尔盆地贝尔凹陷贝48井岩性柱状综合图与碎屑锆石测年样品位置

Fig. 5. Stratigraphic chart of well Bei 48 from the Beier depression in Hailar basin and the sampling location for detrital zircon dating

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图 6 海拉尔盆地晚侏罗世砂岩碎屑锆石年龄谱和代表性锆石阴极发光照片(a~b)和年龄谐和图(c~d)

Fig. 6. Relative age probability plots and CL images (a~b) and concordia diagrams (c~d) of detrital zircons dating for the Late Jurassic sandstones of the Hailar basin

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表 1 海拉尔盆地塔木兰沟组砂岩碎屑锆石U-Pb测年结果

Table 1. Results of detrital zircon U-Pb dating of basal sandstone samples of the Hailar basin

分析测点	²³²Th (10^-6)	²³⁸U (10^-6)	Th/U	同位素比值						同位素年龄(Ma)
				²⁰⁷Pb/²⁰⁶Pb		²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U		²⁰⁷Pb/²⁰⁶Pb		²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U
				比值	1σ	比值	1σ	比值	1σ	年龄	1σ	年龄	1σ	年龄	1σ
B48-1塔木兰沟组
b48-1-01	344	255	1.35	0.048 89	0.003 38	0.146 53	0.010 05	0.021 74	0.000 42	143	157	139	9	139	3
b48-1-02	409	359	1.14	0.050 85	0.003 15	0.136 95	0.008 33	0.019 53	0.000 43	234	143	130	7	125	3
b48-1-03	83	88	0.95	0.053 43	0.002 69	0.403 14	0.020 30	0.054 72	0.000 92	347	117	344	15	343	6
b48-1-04	395	301	1.31	0.049 07	0.002 47	0.161 82	0.008 05	0.023 91	0.000 47	151	115	152	7	152	3
b48-1-05	191	147	1.30	0.049 04	0.004 26	0.159 94	0.013 76	0.023 65	0.000 50	150	197	151	12	151	3
b48-1-06	434	316	1.37	0.048 96	0.002 02	0.162 10	0.006 76	0.024 01	0.000 42	146	96	153	6	153	3
b48-1-07	427	161	2.65	0.051 56	0.002 34	0.298 04	0.013 45	0.041 91	0.000 73	266	107	265	11	265	5
b48-1-08	137	89	1.55	0.053 63	0.003 66	0.391 06	0.026 12	0.052 88	0.001 23	356	158	335	19	332	8
b48-1-09	458	290	1.58	0.048 86	0.002 62	0.146 43	0.007 81	0.021 73	0.000 39	141	122	139	7	139	2
b48-1-10	111	97	1.14	0.048 91	0.006 62	0.147 21	0.019 67	0.021 82	0.000 60	144	276	139	17	139	4
b48-1-11	515	260	1.99	0.048 69	0.003 07	0.147 30	0.009 18	0.021 94	0.000 44	133	142	140	8	140	3
b48-1-12	999	763	1.31	0.048 94	0.001 23	0.154 30	0.004 08	0.022 86	0.000 36	145	60	146	4	146	2
b48-1-13	402	465	0.86	0.048 81	0.001 63	0.148 23	0.005 05	0.022 02	0.000 36	139	78	140	4	140	2
b48-1-14	117	155	0.75	0.049 38	0.003 91	0.154 18	0.012 03	0.022 64	0.000 50	166	180	146	11	144	3
b48-1-15	139	76	1.84	0.057 72	0.008 40	0.181 23	0.025 77	0.022 77	0.000 83	519	327	169	22	145	5
b48-1-16	268	267	1.00	0.051 94	0.002 34	0.325 50	0.014 59	0.045 46	0.000 87	283	106	286	11	287	5
b48-1-17	106	163	0.65	0.049 22	0.003 87	0.152 84	0.011 86	0.022 52	0.000 51	158	179	144	10	144	3
b48-1-18	181	157	1.16	0.049 27	0.003 94	0.165 89	0.013 05	0.024 42	0.000 59	161	182	156	11	156	4
b48-1-19	714	495	1.44	0.048 84	0.001 92	0.156 10	0.006 17	0.023 19	0.000 42	140	91	147	5	148	3
b48-1-20	712	452	1.57	0.048 81	0.002 64	0.135 77	0.007 24	0.020 18	0.000 42	139	123	129	6	129	3
b48-1-21	708	264	2.68	0.048 82	0.003 37	0.147 20	0.009 96	0.021 87	0.000 51	139	156	139	9	139	3
b48-1-22	202	156	1.30	0.049 32	0.004 05	0.159 95	0.012 90	0.023 53	0.000 58	163	186	151	11	150	4
b48-1-23	293	231	1.27	0.049 33	0.002 64	0.171 63	0.009 13	0.025 24	0.000 49	164	122	161	8	161	3
b48-1-24	277	337	0.82	0.048 69	0.001 98	0.149 32	0.006 13	0.022 25	0.000 40	133	94	141	5	142	3
b48-1-25	379	317	1.20	0.048 75	0.002 21	0.143 15	0.006 47	0.021 3	0.000 40	136	104	136	6	136	3
b48-1-26	722	363	1.99	0.048 98	0.002 66	0.132 72	0.007 11	0.019 66	0.000 41	147	124	127	6	126	3
b48-1-27	572	548	1.04	0.049 24	0.001 38	0.166 84	0.004 85	0.024 58	0.000 42	159	67	157	4	157	3
b48-1-28	445	451	0.99	0.049 07	0.002 00	0.153 48	0.006 24	0.022 69	0.000 43	151	95	145	5	145	3
b48-1-29	523	419	1.25	0.048 80	0.001 82	0.146 40	0.005 51	0.021 77	0.000 39	138	87	139	5	139	2
b48-1-30	549	255	2.15	0.048 86	0.002 68	0.148 49	0.008 06	0.022 05	0.000 45	141	125	141	7	141	3
b48-1-31	815	552	1.48	0.048 71	0.001 86	0.149 40	0.005 73	0.022 26	0.000 42	134	88	141	5	142	3
b48-1-32	576	464	1.24	0.049 01	0.001 81	0.155 95	0.005 85	0.023 09	0.000 43	148	87	147	5	147	3
b48-1-33	159	114	1.39	0.049 44	0.004 56	0.154 20	0.013 97	0.022 63	0.000 59	169	209	146	12	144	4
b48-1-34	210	235	0.90	0.049 35	0.003 66	0.160 14	0.011 58	0.023 55	0.000 61	164	168	151	10	150	4
b48-1-35	199	145	1.37	0.048 67	0.004 10	0.165 78	0.013 63	0.024 72	0.000 67	132	190	156	12	157	4
b48-1-36	437	504	0.87	0.049 09	0.001 65	0.161 98	0.005 60	0.023 95	0.000 44	152	80	152	5	153	3
b48-1-38	100	56	1.77	0.052 36	0.009 18	0.172 25	0.029 29	0.023 87	0.001 14	301	357	161	25	152	7
b48-1-39	372	235	1.59	0.048 75	0.002 74	0.146 76	0.008 16	0.021 84	0.000 49	136	127	139	7	139	3
b48-1-40	459	477	0.96	0.048 72	0.002 47	0.149 10	0.007 52	0.022 21	0.000 48	134	116	141	7	142	3
b48-1-41	149	132	1.13	0.049 24	0.003 53	0.165 14	0.011 64	0.024 34	0.000 60	159	163	155	10	155	4
b48-1-42	92	75	1.23	0.049 26	0.006 20	0.157 58	0.019 36	0.023 21	0.000 80	160	267	149	17	148	5
b48-1-43	206	182	1.13	0.049 57	0.002 91	0.186 23	0.010 83	0.027 26	0.000 63	175	134	173	9	173	4
b48-1-44	199	150	1.33	0.053 64	0.003 32	0.370 50	0.022 54	0.050 12	0.001 24	356	143	320	17	315	8
b48-1-45	865	410	2.11	0.051 79	0.002 62	0.185 99	0.009 37	0.026 06	0.000 59	276	119	173	8	166	4
b48-1-37	1 765	419	4.22	0.049 66	0.002 21	0.172 18	0.007 75	0.025 16	0.000 53	179	104	161	7	160	3
b48-1-46	521	401	1.30	0.048 92	0.002 56	0.153 03	0.007 93	0.022 69	0.000 50	144	119	145	7	145	3
b48-1-47	245	235	1.04	0.049 06	0.003 97	0.153 11	0.012 08	0.022 64	0.000 63	151	183	145	11	144	4
b48-1-48	203	177	1.14	0.049 79	0.003 21	0.197 21	0.012 52	0.028 73	0.000 69	185	147	183	11	183	4
b48-1-49	736	644	1.14	0.049 90	0.001 97	0.158 03	0.006 31	0.022 97	0.000 46	190	94	149	6	146	3
b48-1-50	421	207	2.03	0.048 91	0.004 02	0.158 63	0.012 71	0.023 53	0.000 66	144	186	150	11	150	4
b48-1-52	255	168	1.51	0.053 57	0.003 44	0.374 41	0.023 52	0.050 70	0.001 27	353	149	323	17	319	8
b48-1-53	498	568	0.88	0.048 75	0.001 90	0.157 00	0.006 23	0.023 36	0.000 46	136	90	148	5	149	3
b48-1-54	295	206	1.43	0.048 95	0.003 52	0.153 87	0.010 86	0.022 80	0.000 58	145	163	145	10	145	4
b48-1-55	1383	380	3.64	0.049 53	0.003 43	0.141 15	0.009 55	0.020 67	0.000 53	173	158	134	8	132	3
b48-1-56	224	178	1.26	0.049 56	0.005 07	0.155 66	0.015 39	0.022 79	0.000 78	174	229	147	14	145	5
b48-1-57	411	206	1.99	0.049 61	0.003 86	0.155 28	0.011 85	0.022 71	0.000 60	177	177	147	10	145	4
b48-1-59	697	564	1.23	0.048 89	0.002 49	0.150 67	0.007 64	0.022 36	0.000 51	143	116	143	7	143	3
b48-1-60	442	348	1.27	0.048 92	0.003 44	0.146 42	0.010 07	0.021 71	0.000 58	144	159	139	9	138	4
b48-1-58	108	106	1.02	0.048 87	0.004 93	0.156 15	0.015 44	0.023 18	0.000 70	142	226	147	14	148	4
b48-1-51	367	299	1.22	0.048 89	0.002 89	0.152 88	0.008 96	0.022 68	0.000 54	143	134	144	8	145	3
b48-1-61	270	243	1.11	0.049 68	0.007 12	0.155 56	0.022 17	0.022 73	0.000 51	180	291	147	19	145	3
b48-1-62	641	625	1.03	0.048 94	0.002 79	0.150 08	0.008 57	0.022 27	0.000 37	145	130	142	8	142	2
b48-1-63	139	138	1.01	0.049 05	0.010 38	0.152 21	0.032 09	0.022 53	0.000 57	150	380	144	28	144	4
b48-1-64	408	378	1.08	0.052 81	0.002 18	0.370 65	0.015 47	0.050 95	0.000 80	321	96	320	11	320	5
b48-1-65	163	87	1.86	0.050 90	0.011 46	0.260 90	0.058 51	0.037 21	0.001 02	236	410	235	47	236	6
b48-1-66	246	151	1.62	0.049 09	0.009 23	0.157 55	0.029 53	0.023 30	0.000 54	152	346	149	26	148	3
b48-1-68	320	286	1.12	0.048 85	0.004 90	0.150 32	0.015 06	0.022 34	0.000 41	141	224	142	13	142	3
b48-1-69	128	89	1.45	0.048 37	0.021 27	0.132 30	0.057 96	0.019 85	0.000 83	117	755	126	52	127	5
b48-1-70	35	56	0.63	0.054 05	0.011 09	0.395 08	0.080 74	0.053 05	0.001 39	373	401	338	59	333	9
b48-1-71	224	73	3.06	0.050 77	0.017 82	0.160 98	0.056 33	0.023 02	0.000 76	230	611	152	49	147	5
b48-1-72	59	61	0.97	0.049 48	0.022 57	0.160 47	0.072 97	0.023 54	0.000 95	171	798	151	64	150	6
b48-1-73	430	463	0.93	0.049 33	0.003 37	0.155 68	0.010 68	0.022 90	0.000 39	164	155	147	9	146	2
b48-1-74	279	266	1.05	0.049 41	0.005 19	0.169 77	0.017 80	0.024 93	0.000 47	167	236	159	15	159	3
b48-1-75	460	213	2.16	0.049 22	0.007 12	0.150 34	0.021 68	0.022 16	0.000 47	158	290	142	19	141	3
b48-1-76	119	88	1.34	0.053 20	0.007 44	0.396 86	0.055 33	0.054 13	0.001 20	337	313	339	40	340	7
b48-1-67	117	79	1.48	0.048 83	0.035 82	0.132 28	0.096 64	0.019 66	0.001 37	140	1116	126	87	126	9
B48-3塔木兰沟组
b48-3-01	230	124	1.86	0.049 04	0.003 75	0.155 88	0.011 83	0.023 05	0.000 45	150	173	147	10	147	3
b48-3-02	1 073	362	2.96	0.048 87	0.001 99	0.157 47	0.006 42	0.023 37	0.000 41	142	94	148	6	149	3
b48-3-03D	459	413	1.11	0.048 50	0.002 78	0.137 01	0.007 72	0.020 49	0.000 42	124	130	130	7	131	3
b48-3-04D	501	401	1.25	0.048 87	0.001 93	0.151 54	0.006 01	0.022 49	0.000 39	142	92	143	5	143	2
b48-3-05	537	399	1.34	0.049 35	0.001 66	0.160 97	0.005 50	0.023 66	0.000 39	164	80	152	5	151	2
b48-3-06	364	199	1.83	0.049 02	0.002 71	0.158 99	0.008 73	0.023 52	0.000 45	149	126	150	8	150	3
b48-3-07	260	120	2.18	0.049 09	0.004 21	0.149 42	0.012 74	0.022 07	0.000 45	152	194	141	11	141	3
b48-3-09	309	332	0.93	0.048 87	0.001 71	0.152 07	0.005 44	0.022 56	0.000 38	142	82	144	5	144	2
b48-3-10	257	278	0.93	0.048 71	0.002 19	0.143 19	0.006 44	0.021 32	0.000 38	134	103	136	6	136	2
b48-3-11	350	309	1.13	0.049 11	0.002 13	0.163 85	0.007 11	0.024 20	0.000 44	153	101	154	6	154	3
b48-3-12	324	308	1.05	0.049 13	0.001 79	0.161 43	0.005 98	0.023 83	0.000 41	154	86	152	5	152	3
b48-3-13	68	72	0.94	0.049 36	0.006 01	0.172 83	0.020 74	0.025 40	0.000 71	165	258	162	18	162	4
b48-3-14	357	305	1.17	0.048 69	0.002 43	0.163 26	0.008 10	0.024 32	0.000 47	133	114	154	7	155	3
b48-3-08	248	167	1.48	0.048 99	0.003 40	0.153 21	0.010 50	0.022 68	0.000 50	147	157	145	9	145	3
b48-3-15	141	80	1.76	0.050 04	0.008 47	0.157 84	0.026 32	0.022 88	0.000 79	197	324	149	23	146	5
b48-3-16	741	559	1.32	0.049 00	0.001 50	0.157 55	0.004 98	0.023 32	0.000 40	148	73	149	4	149	3
b48-3-17	86	78	1.11	0.049 15	0.006 20	0.161 80	0.020 20	0.023 88	0.000 63	155	265	152	18	152	4
b48-3-18	414	374	1.11	0.049 22	0.002 25	0.167 62	0.007 63	0.024 70	0.000 48	158	106	157	7	157	3
b48-3-19	256	193	1.33	0.049 70	0.002 61	0.188 98	0.009 86	0.027 58	0.000 54	181	122	176	8	175	3
b48-3-20	677	342	1.98	0.049 99	0.003 52	0.159 04	0.010 96	0.023 08	0.000 56	195	161	150	10	147	4
b48-3-21	106	98	1.08	0.048 87	0.005 64	0.151 54	0.017 27	0.022 49	0.000 60	142	250	143	15	143	4
b48-3-22	95	93	1.02	0.049 15	0.004 98	0.161 01	0.016 16	0.023 76	0.000 56	155	227	152	14	151	4
b48-3-23	185	180	1.03	0.049 08	0.003 13	0.159 75	0.010 07	0.023 61	0.000 50	152	145	150	9	150	3
b48-3-24	814	603	1.35	0.049 01	0.001 63	0.149 18	0.005 06	0.022 08	0.000 39	148	79	141	4	141	2
b48-3-25	26	48	0.55	0.048 90	0.008 17	0.156 47	0.025 80	0.023 21	0.000 76	143	314	148	23	148	5
b48-3-26	294	327	0.90	0.048 85	0.002 02	0.149 64	0.006 22	0.022 22	0.000 41	141	96	142	5	142	3
b48-3-27	228	135	1.69	0.049 40	0.004 58	0.175 77	0.015 94	0.025 81	0.000 70	167	211	164	14	164	4
b48-3-28	134	91	1.48	0.050 12	0.006 75	0.168 00	0.022 13	0.024 31	0.000 84	201	281	158	19	155	5
b48-3-29	307	318	0.97	0.048 79	0.002 49	0.149 96	0.007 59	0.022 3	0.000 46	138	116	142	7	142	3
b48-3-30	620	515	1.20	0.049 20	0.001 95	0.167 56	0.006 69	0.024 71	0.000 48	157	93	157	6	157	3
b48-3-31	221	185	1.19	0.049 25	0.003 19	0.169 58	0.010 85	0.024 98	0.000 57	160	147	159	9	159	4
b48-3-32	467	316	1.48	0.049 00	0.002 40	0.161 66	0.007 89	0.023 94	0.000 49	148	112	152	7	153	3
b48-3-33	278	279	1.00	0.049 04	0.002 98	0.159 96	0.009 56	0.023 67	0.000 55	150	138	151	8	151	3
b48-3-34	90	98	0.92	0.049 18	0.005 65	0.169 03	0.019 00	0.024 94	0.000 78	156	252	159	17	159	5
b48-3-35	225	164	1.37	0.048 95	0.003 51	0.159 36	0.011 27	0.023 63	0.000 56	145	162	150	10	151	4
b48-3-36	138	118	1.16	0.049 11	0.004 43	0.158 57	0.014 09	0.023 44	0.000 61	153	204	149	12	149	4
b48-3-37	471	437	1.08	0.048 84	0.002 02	0.152 17	0.006 34	0.022 61	0.000 45	140	96	144	6	144	3
b48-3-38	228	161	1.42	0.049 10	0.003 73	0.163 36	0.012 20	0.024 15	0.000 60	153	172	154	11	154	4
b48-3-39	256	245	1.04	0.049 27	0.002 93	0.164 74	0.009 65	0.024 27	0.000 56	161	136	155	8	155	4
b48-3-40	283	207	1.36	0.048 93	0.004 07	0.151 48	0.012 31	0.022 47	0.000 62	144	188	143	11	143	4
b48-3-41	422	208	2.03	0.049 07	0.004 66	0.152 98	0.014 13	0.022 63	0.000 69	151	216	145	12	144	4
b48-3-42	124	97	1.28	0.048 78	0.006 16	0.147 19	0.018 24	0.021 91	0.000 71	137	262	139	16	140	4
b48-3-43	253	268	0.95	0.049 14	0.003 57	0.161 46	0.011 49	0.023 86	0.000 62	155	165	152	10	152	4
b48-3-44	148	82	1.80	0.049 65	0.008 07	0.171 65	0.027 18	0.025 10	0.001 08	179	315	161	24	160	7
b48-3-45	805	313	2.57	0.053 96	0.007 05	0.177 97	0.023 07	0.023 91	0.000 58	369	295	166	20	152	4
b48-3-46	169	194	0.87	0.051 94	0.011 43	0.154 36	0.033 76	0.021 55	0.000 64	283	413	146	30	137	4
b48-3-49	595	280	2.12	0.048 96	0.005 60	0.156 49	0.017 83	0.023 17	0.000 45	146	247	148	16	148	3
b48-3-50	143	200	0.71	0.049 35	0.007 54	0.160 65	0.024 46	0.023 60	0.000 51	164	308	151	21	150	3
b48-3-51	387	461	0.84	0.053 53	0.004 32	0.177 44	0.014 23	0.024 03	0.000 46	351	185	166	12	153	3
b48-3-52	171	176	0.97	0.049 21	0.008 32	0.150 97	0.025 46	0.022 24	0.000 47	158	318	143	22	142	3
b48-3-54	1 030	394	2.61	0.049 63	0.004 01	0.154 21	0.012 41	0.022 52	0.000 39	178	184	146	11	144	2
b48-3-55	266	187	1.43	0.049 65	0.009 07	0.169 84	0.030 86	0.024 80	0.000 63	179	341	159	27	158	4
b48-3-56	441	283	1.56	0.050 20	0.006 55	0.175 10	0.022 68	0.025 29	0.000 57	204	278	164	20	161	4
b48-3-57	526	457	1.15	0.049 00	0.003 47	0.160 18	0.011 32	0.023 70	0.000 40	148	160	151	10	151	3
b48-3-58	501	453	1.11	0.049 39	0.003 71	0.161 80	0.012 1	0.023 75	0.000 41	166	171	152	11	151	3
b48-3-60	282	353	0.80	0.048 98	0.004 20	0.154 80	0.013 21	0.022 91	0.000 39	147	194	146	12	146	2
b48-3-62	231	202	1.14	0.055 49	0.008 58	0.167 36	0.025 72	0.021 86	0.000 51	432	343	157	22	139	3
b48-3-59	604	267	2.26	0.048 64	0.005 51	0.141 20	0.015 93	0.021 05	0.000 38	131	245	134	14	134	2
b48-3-61	257	259	0.99	0.048 76	0.006 18	0.142 72	0.017 99	0.021 22	0.000 41	136	263	135	16	135	3
b48-3-47	454	346	1.31	0.048 79	0.004 41	0.146 21	0.013 13	0.021 73	0.000 37	138	205	139	12	139	2
b48-3-48	276	311	0.89	0.048 78	0.006 27	0.133 82	0.017 09	0.019 89	0.000 40	137	264	128	15	127	3
b48-3-53	290	383	0.76	0.048 85	0.003 85	0.146 57	0.011 48	0.021 76	0.000 35	141	178	139	10	139	2

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