黄骅坳陷歧口主凹区东营组砂岩物源方向与沉积模式：来自碎屑锆石U-Pb年代学的制约

李长海; 董晓伟; 石倩茹; 官全胜; 张佼杨; 朱华汇; 张明振; 董越崎; 付东立; 杨帆

doi:10.19509/j.cnki.dzkq.tb20240696

黄骅坳陷歧口主凹区东营组砂岩物源方向与沉积模式：来自碎屑锆石U-Pb年代学的制约

doi: 10.19509/j.cnki.dzkq.tb20240696

中国石油大港油田公司，天津 300280

基金项目: 国家科技重大专项“渤海湾超级盆地油气富集规律与新领域勘探关键技术”（2024ZD1400100）;中国石油大港油田公司博士后项目“歧口凹陷断砂耦合形成机制与控藏规律研究”（博057）

详细信息

通讯作者:
E-mail：changhai0912@163.com

中图分类号: P618.13
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- 被引次数: 0
出版历程
- 收稿日期: 2024-11-18
- 录用日期: 2025-06-24
- 修回日期: 2025-06-04
- 网络出版日期: 2025-06-24

Source area and sedimentary model of the sandstone in the Third Member of Dongying Formation in main concave, Qikou Sag, Huanghua Depression: Constraints from detrital zircons U-Pb dating

PetroChina Dagang Oilfield Company, Tianjin 300280, China

More Information

Corresponding author: E-mail：changhai0912@163.com

摘要

摘要:
歧口主凹新部署的HT1井在东营组三亚段（东三段）钻遇一套重力流砂体并获工业油流，取得了主凹区的勘探突破，但是目前对其物源方向和空间展布特征尚不明确，制约了下步勘探工作。基于地震和测录井资料，利用碎屑锆石LA-ICP-MS U-Pb定年方法对歧口主凹区东三段砂岩开展了源−渠−汇约束下的沉积体系研究工作。碎屑锆石U-Pb定年结果表明，歧口主凹东三段砂岩碎屑锆石年龄主要集中在160～100，300～240，2000～1680，2600～2300 Ma 4个年龄区间内，其中160～100 Ma区间年龄峰值明显。盆外物源区沧县隆起FU1X1井东三段砂岩碎屑锆石年龄在二叠纪（300～240 Ma）具有明显峰值。北部燕山造山带发育有从太古宙到中生代的岩浆岩，中生代岩浆作用强烈，160～100 Ma区间的年龄峰值特征明显。HT1井东三段砂岩碎屑锆石年龄特征与燕山造山带年龄峰值特征具有较高一致性，表明北部燕山造山带为其物源区。结合前人轻重矿物研究成果和东三段沉积时期歧口主凹区北高南低的古地貌特征，构建了歧口主凹区东三段砂岩“远源供砂、沟槽输砂、深凹聚砂”的沉积模式。研究成果为后续主凹区井位部署提供了依据。
- 碎屑锆石 /
- U-Pb定年 /
- 歧口凹陷 /
- 沉积模式 /
- 物源
Abstract: Objective
The Qikou Sag, a significant hydrocarbon-bearing sub-basin within the Bohai Bay Basin of eastern China, has recently witnessed a critical exploration breakthrough. Well HT1, drilled in the main trough, encountered a sandstone reservoir within the Third Member of the Dongying Formation (Ed₃) and achieved commercial oil flow. However, the precise provenance and spatial distribution of this Ed₃ sandstone remain enigmatic. Identifying the sediment source is fundamental to constructing a reliable "source-to-sink" system, which is crucial for predicting the distribution of high-quality reservoirs. This study aims to definitively determine the provenance of the Ed₃ sandstone through detrital zircon U-Pb geochronology and establish a robust sedimentary model to guide exploration.
Methods
To address the provenance question, this study employed laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) U-Pb dating on detrital zircons extracted from the Ed₃ sandstone. Zircon is an ideal mineral for provenance analysis due to its high physical and chemical stability, allowing it to survive multiple cycles of erosion and transport while preserving its primary crystallization age. Thus, the age spectrum of detrital zircons in a sedimentary rock serves as a unique fingerprint that can be compared to the age signatures of potential source areas, enabling a direct link between the sediment and its origin.
Results
The U-Pb dating results from the Ed₃ sandstone revealed a characteristic age distribution pattern. The detrital zircon ages cluster into four primary intervals: 2600−2300 Ma (Neoarchean to Paleoproterozoic), 1680−2000 Ma (Paleoproterozoic), 300−240 Ma (Permian), and a remarkably dominant peak between 160−100 Ma (Jurassic to Cretaceous). The overwhelming abundance of zircons in the 160−100 Ma range immediately pointed towards a significant contribution from a source region with intense Mesozoic magmatic activity. The zircon age signature of the Cangxian uplift was examined. Its age spectrum is characterized by a strong peak at 300−240 Ma and a relative lack of Mesozoic zircons, presenting a clear mismatch with the Ed₃ sandstone signature and effectively ruling it out as the primary source. In contrast, the Yanshan orogenic belt to the north is a complex tectonic zone with a prolonged magmatic history spanning from the Archean to the Mesozoic. Critically, it is renowned for widespread Jurassic-Cretaceous (Yanshanian) magmatism, with a pronounced age peak precisely between 160 and 100 Ma. The striking similarity between the Ed₃ zircon age pattern and the magmatic record of the Yanshan belt provides compelling evidence that the latter served as the principal provenance for the sandstone. Previous studies indicate that the Yanshan orogenic belt experienced significant Cenozoic uplift, coeval with the deposition of the Ed₃, creating a well-defined mountain-basin system. Several major paleo-rivers, such as the ancient Yongding River, ancient Chaobai River, and ancient Luan River, are interpreted to have acted as efficient sediment conduits. These rivers eroded the Mesozoic granitic rocks of the Yanshan belt and transported the detritus southward over long distances into the Qikou Sag.
Conclusions
This study successfully resolves the provenance of the Ed₃ sandstone in the main trough of the Qikou Sag. Detrital zircon U-Pb geochronology unequivocally identifies the northern Yanshan orogenic belt as the primary source, excluding the nearby Cangxian uplift. The construction of the "remote source, channelized transport, deep-trough deposition" model has profound implications for exploration. It validates the existence of high-quality sandstone reservoirs in the deep troughs formed by long-distance transport systems. Consequently, future exploration efforts should prioritize mapping the paleo-drainage pathways that funneled sediments from the Yanshan belt into the main trough of the Qikou Sag. This model significantly reduces exploration risk in the deep plays of the depression and provides a valuable analog for searching for similar subtle reservoirs in other continental rift basins worldwide.
- detrital zircon /
- U-Pb age dating /
- Qikou Sag /
- sedimentation model /
- source

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图 1 渤海湾盆地区域构造图（a）和歧口凹陷构造分区图（b）（据文献[7，9]修改）

Figure 1. Regional tectonical map of Bohai Bay Basin (a) and tectonical division map of Qikou Sag (b)

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图 2 歧口凹陷新生界综合地层柱状图

Figure 2. Comprehensive stratigraphic column of Cenozoic in Qikou Sag

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图 3 HT1井（a）与FU1X1井（b）东三段取样层位（SP. 自然电位；GR. 自然伽马）

Figure 3. Sample positions in Ed₃ of Well HT1 (a) and Well FU1X1 (b)

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图 4 代表性锆石CL图（红圈为激光打点位置，下方为该点年龄，括号内数字为数据点号）

Figure 4. Representative detrital zircons CL images

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图 5 碎屑锆石样品Th/U比值散点图

Figure 5. Th/U ratios of the detrital zircons

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图 6 碎屑锆石年龄频数分布直方图（左列为各样品所有样品点，右列为虚线框内柱状图详细特征）

Figure 6. Binned frequency histograms of detrital zircons U-Pb ages

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图 7 燕山物源(a)、沧县物源(b)与HT1井(c)锆石年龄频谱对比图（n. 锆石总数）

Figure 7. Compared frequency histograms for Yanshan (a), Cangxian (b) sources and Well HT1 (c)

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图 8 歧口凹陷东三段砂地比图

Figure 8. Sand ratio of Ed₃ in Qikou Sag

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图 9 华北古近纪−新近纪水系与燕山地区岩浆岩空间分布图^[43]

Figure 9. Spatial distribution of Paleogene drainage in Huabei and igneous rocks in Yanshan area

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图 10 过HT1井SN向地震剖面图（剖面位置见图1）

Nm. 明化镇组；Ng. 馆陶组；Ed. 东营组；Es₁. 沙一段；Es₂. 沙二段；Es₃. 沙三段

Figure 10. SN seismic profile crossing Well HT1

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图 11 歧口凹陷东三段振幅属性图（a）和古地貌图（b）

Figure 11. Amplitude attribute (a) and the palaeotopography (b) of Ed₃ in Qikou Sag

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图 12 歧口凹陷东三段沉积体系图

Figure 12. Sedimentary system of Ed₃ in Qikou Sag

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表 1 碎屑锆石LA-ICP-MS U-Pb定年数据（σ. 误差）

Table 1. Detrital zircons LA-ICP-MS U-Pb dating data

样品及数据点编号	Th	U	Th/U	同位素比值						年龄t/Ma						谐和度/%
样品及数据点编号	w_B/10⁻⁶		Th/U	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	谐和度/%
HT4162
1	664	578	1.15	0.0482	0.0007	0.1300	0.0021	0.0195	0.0002	108	34	124	2	125	1	99
2	312	223	1.40	0.0492	0.0011	0.1653	0.0039	0.0243	0.0002	158	54	155	3	155	2	100
3	816	528	1.55	0.0520	0.0006	0.3263	0.0042	0.0455	0.0004	286	28	287	3	287	2	100
4	721	544	1.33	0.0508	0.0010	0.2348	0.0041	0.0336	0.0004	233	45	214	3	213	3	100
5	46.1	60.9	0.76	0.1654	0.0017	10.9159	0.1018	0.4784	0.0035	2512	17	2516	9	2520	15	100
6	186	161	1.16	0.0488	0.0015	0.1370	0.0044	0.0204	0.0003	137	73	130	4	130	2	100
7	226	318	0.71	0.0517	0.0013	0.1557	0.0037	0.0219	0.0002	274	59	147	3	140	1	95
8	414	850	0.49	0.0493	0.0006	0.1668	0.0023	0.0245	0.0002	161	29	157	2	156	1	100
9	40.1	99.6	0.40	0.1387	0.0013	7.5183	0.0796	0.3925	0.0028	2211	17	2175	10	2135	13	98
10	77.0	187	0.41	0.1171	0.0015	5.6146	0.0758	0.3463	0.0026	1913	24	1918	12	1917	13	100
11	504	358	1.41	0.0488	0.0013	0.1332	0.0039	0.0198	0.0002	138	64	127	4	126	2	100
12	108	111	0.97	0.0490	0.0029	0.1317	0.0076	0.0197	0.0004	147	141	126	7	125	2	100
13	174	199	0.87	0.0510	0.0012	0.2838	0.0073	0.0403	0.0004	242	55	254	6	255	3	100
14	163	179	0.91	0.0491	0.0015	0.1521	0.0046	0.0225	0.0003	153	71	144	4	143	2	100
15	304	244	1.25	0.1178	0.0010	5.3014	0.0536	0.3269	0.0033	1923	16	1869	9	1824	16	98
16	480	433	1.11	0.0589	0.0019	0.1470	0.0037	0.0184	0.0003	561	69	139	3	117	2	84
17	291	246	1.18	0.0492	0.0015	0.1460	0.0047	0.0215	0.0002	158	70	138	4	137	1	99
18	230	344	0.67	0.0491	0.0011	0.1394	0.0031	0.0206	0.0002	152	53	133	3	132	1	99
19	44.3	30.3	1.46	0.1664	0.0015	10.9227	0.1250	0.4760	0.0043	2522	15	2517	11	2510	19	100
20	61.8	79.7	0.78	0.1703	0.0018	11.4655	0.1166	0.4885	0.0034	2561	17	2562	10	2564	15	100
21	324	316	1.03	0.0486	0.0013	0.1355	0.0041	0.0202	0.0002	127	62	129	4	129	2	100
22	84.4	142	0.59	0.1652	0.0018	10.7842	0.1139	0.4727	0.0045	2510	19	2505	10	2496	20	100
23	276	271	1.02	0.0485	0.0013	0.1380	0.0036	0.0207	0.0002	123	62	131	3	132	1	100
24	85.5	275	0.31	0.1115	0.0009	4.7631	0.0361	0.3100	0.0022	1824	14	1778	6	1741	11	98
25	305	243	1.26	0.0514	0.0011	0.2834	0.0069	0.0400	0.0004	260	50	253	5	253	2	100
26	184	375	0.49	0.1666	0.0008	10.8323	0.0744	0.4718	0.0034	2524	8	2509	6	2492	15	99
27	1.09	4.14	0.26	0.1731	0.0043	10.9248	0.2412	0.4639	0.0078	2588	42	2517	21	2457	34	98
28	87.2	164	0.53	0.0525	0.0010	0.3539	0.0079	0.0489	0.0005	306	45	308	6	308	3	100
29	60	74.7	0.80	0.1664	0.0018	10.9573	0.1128	0.4780	0.0032	2521	18	2520	10	2519	14	100
30	102	127	0.80	0.1108	0.0008	4.9213	0.0470	0.3219	0.0026	1813	12	1806	8	1799	13	100
31	493	519	0.95	0.0493	0.0009	0.1593	0.0027	0.0235	0.0002	162	42	150	2	150	1	100
32	93.9	206	0.46	0.0483	0.0016	0.1198	0.0040	0.0181	0.0002	112	79	115	4	115	1	100
33	187	230	0.81	0.0498	0.0014	0.1579	0.0039	0.0231	0.0003	187	66	149	4	148	2	99
34	29.2	32.5	0.90	0.1591	0.0016	9.7166	0.1111	0.4431	0.0036	2446	17	2408	11	2364	16	98
35	71.3	61.8	1.15	0.0497	0.0024	0.1347	0.0062	0.0199	0.0003	180	111	128	6	127	2	99
36	39	61	0.64	0.1652	0.0021	11.0167	0.1527	0.4840	0.0048	2510	22	2525	13	2545	21	99
37	88.1	118	0.75	0.1115	0.0010	4.5109	0.0397	0.2935	0.0015	1825	16	1733	7	1659	8	96
38	34.4	222	0.15	0.1131	0.0013	5.2332	0.0762	0.3353	0.0034	1849	21	1858	12	1864	16	100
39	84	100	0.84	0.0492	0.0024	0.1383	0.0066	0.0205	0.0003	157	112	132	6	131	2	100
40	113	223	0.51	0.0519	0.0013	0.2935	0.0071	0.0412	0.0004	280	59	261	6	260	2	100
41	52.1	128	0.41	0.1661	0.0019	10.4526	0.1464	0.4570	0.0046	2519	19	2476	13	2426	20	98
42	90.2	109	0.83	0.1137	0.0010	5.1511	0.0561	0.3288	0.0028	1859	15	1845	9	1833	14	99
43	594	549	1.08	0.0513	0.0008	0.2713	0.0047	0.0383	0.0004	256	35	244	4	243	2	99
44	90.3	86.4	1.05	0.0484	0.0025	0.1365	0.0072	0.0205	0.0003	119	120	130	6	131	2	99
45	50.8	117	0.43	0.0489	0.0019	0.1392	0.0055	0.0207	0.0003	145	93	132	5	132	2	100
46	102	201	0.51	0.0488	0.0019	0.1205	0.0049	0.0180	0.0002	140	93	116	4	115	2	99
47	80.4	129	0.62	0.0526	0.0013	0.3550	0.0094	0.0490	0.0005	310	55	308	7	308	3	100
48	29.8	28.2	1.06	0.0863	0.0064	0.2906	0.0197	0.0249	0.0007	1345	144	259	16	158	5	61
49	88.9	101	0.88	0.1658	0.0015	10.2421	0.0923	0.4482	0.0035	2515	15	2457	8	2387	15	97
50	260	84.9	3.06	0.1654	0.0011	10.8862	0.0941	0.4767	0.0032	2512	11	2514	8	2513	14	100
51	247	282	0.88	0.0512	0.0011	0.2832	0.0061	0.0402	0.0003	251	48	253	5	254	2	100
52	30.8	172	0.18	0.1649	0.0015	10.3224	0.1364	0.4546	0.0065	2507	16	2464	12	2416	29	98
53	75.9	210	0.36	0.1649	0.0017	9.5995	0.1226	0.4229	0.0039	2507	18	2397	12	2274	18	95
54	114	210	0.54	0.1665	0.0018	11.0031	0.1495	0.4801	0.0045	2523	18	2523	13	2528	20	100
55	97.3	155	0.63	0.0501	0.0019	0.1684	0.0065	0.0246	0.0003	199	89	158	6	156	2	99
56	78.9	233	0.34	0.1119	0.0013	4.5996	0.0614	0.2987	0.0022	1831	22	1749	11	1685	11	96
57	59.6	111	0.54	0.0525	0.0014	0.3745	0.0099	0.0519	0.0005	307	58	323	7	326	3	99
58	517	428	1.21	0.0497	0.0010	0.1955	0.0042	0.0286	0.0002	179	46	181	4	182	2	100
59	310	303	1.02	0.0515	0.0010	0.2840	0.0061	0.0401	0.0004	261	43	254	5	254	3	100
60	230	392	0.59	0.0514	0.0013	0.2819	0.0077	0.0398	0.0004	257	60	252	6	252	3	100
HT4177
1	113	101	1.12	0.0482	0.0021	0.1341	0.0057	0.0202	0.0003	108	104	128	5	129	2	99
2	84.5	108	0.78	0.1119	0.0011	5.0003	0.0495	0.3241	0.0031	1831	17	1819	8	1810	15	99
3	39.7	66	0.60	0.1695	0.0014	11.2128	0.1116	0.4793	0.0044	2553	14	2541	9	2524	19	99
4	223	278	0.80	0.0521	0.0008	0.3370	0.0061	0.0468	0.0004	289	34	295	5	295	3	100
5	175	277	0.63	0.0521	0.0009	0.3201	0.0060	0.0446	0.0004	291	40	282	5	281	3	100
6	94	123	0.76	0.1870	0.0022	13.5432	0.1569	0.5267	0.0051	2716	19	2718	11	2727	21	100
7	89.8	188	0.48	0.0493	0.0018	0.1491	0.0053	0.0220	0.0002	162	83	141	5	140	2	99
8	151	219	0.69	0.0483	0.0014	0.1331	0.0040	0.0200	0.0002	116	67	127	4	128	1	100
9	21.2	43.1	0.49	0.1065	0.0014	4.6094	0.0760	0.3142	0.0038	1740	24	1751	14	1762	19	99
10	301	520	0.58	0.0485	0.0010	0.1170	0.0024	0.0175	0.0002	125	47	112	2	112	1	100
11	151	229	0.66	0.0524	0.0011	0.3055	0.0066	0.0424	0.0005	304	47	271	5	268	3	99
12	170	230	0.74	0.1121	0.0009	5.0596	0.0640	0.3274	0.0029	1833	15	1829	11	1826	14	100
13	56	161	0.35	0.0738	0.0008	1.7545	0.0236	0.1725	0.0015	1035	21	1029	9	1026	8	100
14	76.2	65.2	1.17	0.0550	0.0018	0.1970	0.0071	0.0262	0.0005	413	74	183	6	166	3	91
15	93.9	177	0.53	0.0481	0.0020	0.1222	0.0053	0.0184	0.0002	103	99	117	5	118	1	99
16	54.5	119	0.46	0.1522	0.0022	9.3829	0.1725	0.4460	0.0068	2371	24	2376	17	2377	30	100
17	85	204	0.42	0.1664	0.0017	10.1168	0.1554	0.4421	0.0059	2521	18	2446	14	2360	26	97
18	57.1	73.9	0.77	0.0498	0.0027	0.1261	0.0069	0.0184	0.0003	187	124	121	6	118	2	98
19	119	127	0.94	0.0499	0.0019	0.1414	0.0053	0.0208	0.0003	190	90	134	5	132	2	99
20	127	294	0.43	0.1650	0.0014	10.7104	0.1085	0.4712	0.0040	2507	15	2498	9	2489	18	100
21	78.6	124	0.63	0.1663	0.0016	10.4863	0.0982	0.4581	0.0037	2521	16	2479	9	2431	16	98
22	40.9	94.8	0.43	0.1164	0.0010	5.5468	0.0516	0.3458	0.0023	1902	15	1908	8	1915	11	100
23	101	159	0.64	0.1122	0.0015	5.1147	0.0722	0.3311	0.0028	1835	24	1839	12	1844	14	100
24	420	758	0.55	0.0554	0.0007	0.3561	0.0053	0.0467	0.0004	428	30	309	4	294	2	95
25	66.4	109	0.61	0.0604	0.0025	0.1797	0.0073	0.0217	0.0003	619	89	168	6	138	2	83
26	39.4	34.4	1.15	0.1549	0.0025	9.1773	0.1387	0.4312	0.0046	2400	27	2356	14	2311	21	98
27	117	49.7	2.35	0.1655	0.0017	10.7806	0.1355	0.4736	0.0046	2513	17	2504	12	2499	20	100
28	132	277	0.48	0.1177	0.0010	4.9624	0.0493	0.3067	0.0025	1921	16	1813	8	1724	12	95
29	79.5	197	0.40	0.1064	0.0018	4.5841	0.0796	0.3132	0.0030	1739	32	1746	15	1756	15	99
30	61.2	56.1	1.09	0.1667	0.0017	10.8507	0.1380	0.4733	0.0043	2525	17	2510	12	2498	19	100
31	563	338	1.67	0.0493	0.0011	0.1692	0.0040	0.0249	0.0002	161	51	159	4	159	1	100
32	48.2	229	0.21	0.1059	0.0010	2.8617	0.0347	0.1961	0.0013	1730	18	1372	9	1155	7	84
33	258	256	1.01	0.0527	0.0009	0.3505	0.0061	0.0484	0.0005	315	39	305	5	305	3	100
34	35.5	41.3	0.86	0.1650	0.0018	10.7582	0.1300	0.4732	0.0049	2508	19	2503	11	2498	21	100
35	88.9	105	0.85	0.0530	0.0016	0.3505	0.0098	0.0482	0.0006	328	67	305	7	304	3	100
36	25.6	46.5	0.55	0.1656	0.0020	10.8869	0.1418	0.4769	0.0039	2514	20	2514	12	2514	17	100
37	51.9	95.5	0.54	0.0565	0.0012	0.5619	0.0108	0.0728	0.0007	470	49	453	7	453	5	100
38	290	333	0.87	0.1647	0.0020	10.3777	0.1178	0.4561	0.0038	2505	20	2469	11	2422	17	98
39	282	449	0.63	0.0512	0.0008	0.2892	0.0051	0.0409	0.0005	248	36	258	4	259	3	100
40	232	355	0.65	0.1543	0.0012	9.2988	0.1087	0.4366	0.0042	2394	13	2368	11	2336	19	99
41	104	99.7	1.04	0.1704	0.0016	11.4803	0.1594	0.4879	0.0056	2561	15	2563	13	2562	24	100
42	28.1	31.1	0.90	0.1656	0.0022	11.0063	0.1947	0.4806	0.0055	2514	22	2524	17	2530	24	100
43	68	88.5	0.77	0.1119	0.0011	5.1763	0.0627	0.3352	0.0031	1831	18	1849	10	1864	15	99
44	107	305	0.35	0.1615	0.0012	9.7019	0.0812	0.4355	0.0030	2471	13	2407	8	2331	13	97
45	52.7	149	0.35	0.1693	0.0015	11.3500	0.1209	0.4864	0.0036	2551	15	2552	10	2555	16	100
46	1300	830	1.57	0.0491	0.0014	0.1235	0.0036	0.0183	0.0002	153	67	118	3	117	1	99
47	243	234	1.04	0.0517	0.0012	0.2930	0.0073	0.0410	0.0004	272	53	261	6	259	2	99
48	180	214	0.84	0.1650	0.0014	10.3367	0.1167	0.4543	0.0042	2508	15	2465	11	2414	19	98
49	176	333	0.53	0.0511	0.0010	0.2863	0.0063	0.0406	0.0004	244	46	256	5	257	2	100
50	102	166	0.61	0.1143	0.0011	5.3905	0.0702	0.3412	0.0032	1869	18	1883	11	1892	15	100
51	151	194	0.78	0.0576	0.0016	0.1684	0.0048	0.0212	0.0002	515	59	158	4	135	1	86
52	120	238	0.50	0.1660	0.0019	10.8792	0.1657	0.4753	0.0044	2518	19	2513	14	2507	19	100
53	53.9	377	0.14	0.1122	0.0012	5.1409	0.0666	0.3319	0.0033	1836	20	1843	11	1848	16	100
54	236	94.8	2.49	0.1324	0.0120	0.4528	0.0475	0.0238	0.0006	2130	159	379	33	152	4	40
55	210	369	0.57	0.0479	0.0011	0.1364	0.0034	0.0207	0.0002	93	56	130	3	132	1	98
56	338	357	0.95	0.0489	0.0012	0.1523	0.0038	0.0226	0.0003	142	56	144	3	144	2	100
57	26.2	39.5	0.66	0.1651	0.0023	11.1150	0.1941	0.4879	0.0064	2508	23	2533	16	2562	28	99
58	79	162	0.49	0.1658	0.0019	10.9577	0.1690	0.4795	0.0049	2516	20	2520	14	2525	22	100
59	473	500	0.95	0.1607	0.0011	8.8104	0.0970	0.3972	0.0027	2463	12	2319	10	2156	13	93
60	145	236	0.61	0.0700	0.0007	1.4917	0.0214	0.1545	0.0014	929	22	927	9	926	8	100
HT4209
1	38.4	47.2	0.81	0.1647	0.0019	10.8036	0.1283	0.4758	0.0042	2504	20	2506	11	2509	18	100
2	109	160	0.68	0.1314	0.0015	7.0197	0.0720	0.3877	0.0033	2117	21	2114	9	2112	15	100
3	139	516	0.27	0.1118	0.0012	5.1156	0.0582	0.3317	0.0030	1829	19	1839	10	1847	15	100
4	33.7	39.3	0.86	0.1588	0.0022	10.2504	0.1431	0.4680	0.0050	2443	23	2458	13	2475	22	99
5	202	234	0.86	0.1653	0.0019	10.7690	0.1167	0.4728	0.0040	2511	19	2503	10	2496	18	100
6	22.7	23.8	0.95	0.1478	0.0021	8.6167	0.1265	0.4234	0.0043	2320	25	2298	13	2276	19	99
7	46.4	133	0.35	0.1321	0.0014	6.8424	0.0643	0.3764	0.0035	2126	18	2091	8	2059	17	98
8	120	141	0.85	0.0507	0.0015	0.2921	0.0095	0.0417	0.0005	227	68	260	8	264	3	99
9	115	331	0.35	0.1653	0.0015	10.8514	0.0916	0.4768	0.0042	2511	15	2511	8	2513	18	100
10	49.5	656	0.08	0.1318	0.0011	6.2908	0.0481	0.3465	0.0025	2122	15	2017	7	1918	12	95
11	109	244	0.45	0.0496	0.0015	0.1380	0.0040	0.0203	0.0002	178	72	131	4	129	2	99
12	136	160	0.85	0.1123	0.0010	5.1169	0.0428	0.3310	0.0026	1836	16	1839	7	1843	13	100
13	182	222	0.82	0.0487	0.0013	0.1209	0.0031	0.0181	0.0002	133	65	116	3	116	1	100
14	97.2	129	0.75	0.0487	0.0016	0.1661	0.0052	0.0249	0.0003	134	77	156	5	158	2	98
15	64.1	72.7	0.88	0.1520	0.0014	9.3104	0.0939	0.4447	0.0034	2369	16	2369	9	2372	15	100
16	28.6	208	0.14	0.1649	0.0017	10.9274	0.1339	0.4811	0.0049	2507	17	2517	11	2532	21	99
17	95.8	164	0.58	0.1125	0.0008	5.1295	0.0527	0.3311	0.0031	1840	13	1841	9	1844	15	100
18	22.3	32	0.70	0.1664	0.0020	10.8105	0.1854	0.4718	0.0071	2522	20	2507	16	2491	31	99
19	83.9	222	0.38	0.0512	0.0011	0.2794	0.0061	0.0397	0.0003	250	50	250	5	251	2	100
20	87.8	178	0.49	0.1598	0.0014	9.9056	0.1132	0.4498	0.0044	2454	15	2426	11	2394	20	99
21	92.3	69.5	1.33	0.0493	0.0026	0.1365	0.0070	0.0202	0.0004	163	124	130	6	129	2	99
22	40.4	59.6	0.68	0.0517	0.0022	0.2964	0.0129	0.0418	0.0006	273	99	264	10	264	4	100
23	275	263	1.05	0.0722	0.0008	1.5734	0.0188	0.1583	0.0013	990	23	960	7	947	7	99
24	343	258	1.33	0.0505	0.0013	0.1616	0.0043	0.0232	0.0003	219	58	152	4	148	2	97
25	299	371	0.81	0.0518	0.0010	0.3093	0.0064	0.0435	0.0006	276	45	274	5	274	4	100
26	84.6	115	0.74	0.1160	0.0016	5.4193	0.0730	0.3390	0.0029	1895	24	1888	12	1882	14	100
27	341	308	1.11	0.0494	0.0017	0.1386	0.0046	0.0204	0.0003	167	79	132	4	130	2	99
28	147	330	0.45	0.1673	0.0015	10.5373	0.1763	0.4564	0.0066	2531	15	2483	16	2424	29	98
29	156	180	0.87	0.1650	0.0016	10.8834	0.1032	0.4783	0.0033	2508	17	2513	9	2520	15	100
30	340	306	1.11	0.0505	0.0009	0.2419	0.0049	0.0347	0.0003	218	43	220	4	220	2	100
31	15.2	18.4	0.83	0.1728	0.0039	11.9152	0.2961	0.4981	0.0061	2585	37	2598	23	2606	26	100
32	296	370	0.80	0.1653	0.0015	10.6687	0.1198	0.4678	0.0043	2510	16	2495	10	2474	19	99
33	420	288	1.46	0.0539	0.0010	0.4441	0.0085	0.0597	0.0005	366	41	373	6	374	3	100
34	75.3	82.1	0.92	0.1143	0.0016	5.3889	0.0838	0.3420	0.0045	1869	25	1883	13	1896	22	99
35	303	604	0.50	0.0487	0.0009	0.1234	0.0022	0.0184	0.0002	131	43	118	2	118	1	100
36	1300	1310	0.99	0.0490	0.0006	0.1559	0.0023	0.0230	0.0002	150	31	147	2	147	1	100
37	40	65.9	0.61	0.1698	0.0021	11.6372	0.1782	0.4973	0.0065	2555	20	2576	14	2602	28	99
38	16.3	40.6	0.40	0.1042	0.0015	4.3786	0.0610	0.3052	0.0029	1701	26	1708	12	1717	14	100
39	84.1	82.4	1.02	0.1652	0.0022	10.7736	0.1461	0.4726	0.0049	2509	23	2504	13	2495	22	100
40	74.8	96.5	0.78	0.1128	0.0011	4.7876	0.0536	0.3078	0.0027	1845	17	1783	9	1730	13	97
41	470	277	1.70	0.0511	0.0010	0.2726	0.0049	0.0387	0.0004	247	43	245	4	245	2	100
42	2.19	28.1	0.08	0.1123	0.0031	5.1844	0.1299	0.3358	0.0041	1838	50	1850	21	1867	20	99
43	27.3	30.3	0.90	0.1608	0.0023	10.1664	0.1313	0.4599	0.0045	2464	25	2450	12	2439	20	100
45	122	157	0.78	0.1123	0.0009	5.0651	0.0516	0.3269	0.0028	1836	14	1830	9	1823	14	100
46	1190	823	1.45	0.1698	0.0016	5.5253	0.0953	0.2359	0.0037	2556	16	1905	15	1365	20	72
47	226	169	1.34	0.1579	0.0019	8.5597	0.1155	0.3928	0.0042	2433	20	2292	12	2136	19	93
48	35.8	40.2	0.89	0.1071	0.0014	4.6152	0.0684	0.3125	0.0034	1751	24	1752	12	1753	17	100
49	349	927	0.38	0.0510	0.0007	0.2931	0.0051	0.0417	0.0005	242	33	261	4	263	3	99
50	66.6	91.1	0.73	0.1125	0.0014	5.0807	0.0648	0.3278	0.0032	1840	22	1833	11	1828	16	100
51	126	74	1.70	0.0493	0.0027	0.1314	0.0069	0.0195	0.0003	164	126	125	6	124	2	99
52	105	173	0.61	0.0541	0.0018	0.4862	0.0146	0.0655	0.0010	373	75	402	10	409	6	98
53	111	358	0.31	0.1536	0.0012	9.2212	0.0606	0.4356	0.0033	2387	13	2360	6	2331	15	99
54	78.4	62.7	1.25	0.1653	0.0017	10.9929	0.1449	0.4821	0.0049	2511	18	2523	12	2536	21	99
55	51.8	76.4	0.68	0.1193	0.0012	5.7875	0.0740	0.3517	0.0034	1945	19	1945	11	1943	16	100
56	87.3	147	0.59	0.1120	0.0012	5.0128	0.0612	0.3243	0.0027	1833	19	1822	10	1811	13	99
57	320	337	0.95	0.0512	0.0009	0.2801	0.0057	0.0396	0.0004	251	42	251	5	251	2	100
58	325	346	0.94	0.1649	0.0025	8.1146	0.1964	0.3570	0.0071	2506	25	2244	22	1968	34	88
59	539	549	0.98	0.0493	0.0012	0.1578	0.0043	0.0233	0.0003	160	58	149	4	148	2	100
60	66.8	90.1	0.74	0.1586	0.0016	9.9241	0.1373	0.4531	0.0045	2441	17	2428	13	2409	20	99
FU1680
1	113	93.6	1.20	0.1631	0.0022	10.2734	0.1581	0.4565	0.0045	2487	23	2460	14	2424	20	98%
2	380	303	1.25	0.0560	0.0017	0.3179	0.0086	0.0415	0.0005	450	67	280	7	262	3	93%
3	338	194	1.74	0.0501	0.0026	0.1478	0.0076	0.0215	0.0003	211	119	140	7	137	2	97%
5	54.0	43.5	1.24	0.1629	0.0022	12.0152	0.2075	0.5352	0.0075	2487	23	2606	16	2763	31	94%
6	79.8	218	0.37	0.1571	0.0018	9.2581	0.1239	0.4271	0.0041	2424	19	2364	12	2293	18	96%
8	147	171	0.86	0.0530	0.0019	0.2700	0.0096	0.0371	0.0004	332	77	243	8	235	2	96%
10	373	467	0.80	0.0526	0.0013	0.2582	0.0067	0.0355	0.0004	322	54	233	5	225	2	96%
11	213	738	0.29	0.0515	0.0010	0.2805	0.0064	0.0394	0.0004	265	46	251	5	249	3	99%
12	58.0	110	0.53	0.0550	0.0024	0.3841	0.0161	0.0512	0.0007	413	92	330	12	322	4	97%
13	270	448	0.60	0.0530	0.0014	0.3314	0.0081	0.0455	0.0004	328	27	291	6	287	3	98%
14	323	263	1.23	0.0591	0.0014	0.4832	0.0117	0.0592	0.0006	572	50	400	8	371	4	92%
15	117	112	1.05	0.0543	0.0033	0.1578	0.0093	0.0214	0.0004	383	140	149	8	137	2	91%
16	190	158	1.21	0.0553	0.0019	0.3190	0.0111	0.0419	0.0005	433	76	281	9	264	3	93%
17	87.1	154	0.57	0.0533	0.0027	0.1774	0.0088	0.0244	0.0003	339	117	166	8	155	2	93%
19	278	241	1.15	0.0509	0.0017	0.2716	0.0088	0.0388	0.0005	235	71	244	7	246	3	99%
20	286	212	1.35	0.0540	0.0018	0.2888	0.0097	0.0388	0.0005	372	79	258	8	245	3	95%
21	96.4	129	0.75	0.0540	0.0023	0.3424	0.0137	0.0461	0.0005	372	94	299	10	290	3	97%
22	104	138	0.75	0.1118	0.0016	5.0801	0.0723	0.3285	0.0026	1829	26	1833	12	1831	12	99%
24	158	259	0.61	0.0547	0.0015	0.3595	0.0103	0.0475	0.0004	467	58	312	8	299	3	95%
25	156	200	0.78	0.1697	0.0020	11.7356	0.1925	0.5000	0.0068	2554	19	2584	15	2614	29	98%
26	296	142	2.08	0.0534	0.0020	0.2891	0.0107	0.0394	0.0004	343	85	258	8	249	3	96%
27	0.12	9.85	0.01	0.1222	0.0043	6.7049	0.2471	0.3995	0.0069	1989	62	2073	33	2167	32	95%
28	452	300	1.51	0.0484	0.0018	0.1688	0.0064	0.0253	0.0003	117	89	158	6	161	2	98%
30	37.9	66.4	0.57	0.0545	0.0025	0.3479	0.0161	0.0462	0.0007	394	106	303	12	291	4	95%
31	125	327	0.38	0.0513	0.0013	0.3034	0.0082	0.0428	0.0005	254	64	269	6	270	3	99%
32	135	181	0.74	0.0538	0.0016	0.3444	0.0102	0.0465	0.0005	365	69	300	8	293	3	97%
33	35.2	46.2	0.76	0.0553	0.0036	0.3459	0.0229	0.0457	0.0008	433	146	302	17	288	5	95%
34	180	252	0.71	0.0540	0.0014	0.3413	0.0092	0.0458	0.0005	369	59	298	7	289	3	96%
35	63.0	257	0.24	0.1162	0.0015	5.4812	0.0755	0.3417	0.0032	1898	22	1898	12	1895	15	99%
36	118	294	0.40	0.1117	0.0014	4.4985	0.0644	0.2915	0.0028	1828	22	1731	12	1649	14	95%
37	49.6	338	0.15	0.1118	0.0013	5.0175	0.0639	0.3249	0.0025	1829	21	1822	11	1814	12	99%
38	152	201	0.76	0.1699	0.0020	10.6750	0.1306	0.4552	0.0035	2556	20	2495	11	2418	16	96%
39	251	441	0.57	0.0548	0.0014	0.2748	0.0070	0.0363	0.0003	406	57	247	6	230	2	93%
40	153	221	0.69	0.0522	0.0016	0.3152	0.0093	0.0439	0.0005	295	64	278	7	277	3	99%
42	190	200	0.95	0.0545	0.0014	0.4571	0.0119	0.0608	0.0006	394	53	382	8	381	3	99%
43	109	170	0.64	0.0653	0.0014	1.1762	0.0261	0.1307	0.0013	783	44	790	12	792	8	99%
44	37.8	67.9	0.56	0.1827	0.0024	12.7475	0.2090	0.5046	0.0053	2677	21	2661	15	2634	23	98%
45	90.9	472	0.19	0.1128	0.0013	4.7650	0.0551	0.3058	0.0020	1856	20	1779	10	1720	10	96%
47	84.9	622	0.14	0.0707	0.0009	1.3663	0.0185	0.1398	0.0008	950	26	875	8	843	5	96%
48	89.9	78.2	1.15	0.1534	0.0021	9.3683	0.1301	0.4424	0.0038	2384	23	2375	13	2361	17	99%
49	503	646	0.78	0.0568	0.0010	0.3781	0.0067	0.0483	0.0005	487	34	326	5	304	3	93%
50	510	462	1.11	0.0544	0.0010	0.4314	0.0082	0.0575	0.0005	387	43	364	6	360	3	98%
52	87.9	95.6	0.92	0.0932	0.0016	3.4621	0.0585	0.2695	0.0028	1492	33	1519	13	1538	14	98%
54	50.4	65.4	0.77	0.1101	0.0019	4.1498	0.0725	0.2732	0.0028	1811	32	1664	14	1557	14	93%
55	139	358	0.39	0.0511	0.0012	0.3447	0.0087	0.0489	0.0005	243	56	301	7	308	3	97%
57	266	494	0.54	0.0531	0.0011	0.2991	0.0065	0.0408	0.0003	332	53	266	5	258	2	96%
58	99.4	99.3	1.00	0.0530	0.0025	0.2882	0.0147	0.0392	0.0005	328	107	257	12	248	3	96%
59	97.9	176	0.56	0.1055	0.0016	3.7968	0.0623	0.2603	0.0029	1724	28	1592	13	1491	15	93%
60	155	212	0.73	0.0568	0.0016	0.3406	0.0091	0.0435	0.0005	483	61	298	7	275	3	91%

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