Geochemical Characteristics and Geological Implications of Sandstones in Muling Formation of Lower Cretaceous, Laoheishan Basin, Heilongjiang Province

doi:10.19657/j.geoscience.1000-8527.2018.04.15

Abstract

Abstract:

The Laoheishan Basin is located in Heilongjiang Province, northeast of China, the coal and oil shale are developed in Muling Formation of Lower Cretaceous. Systematic sampling was made and sandstones of Muling Formation in the Laoheishan Basin were analyzed. The results show that the major elements of sandstones in Muling Formation has the characteristics of Fe₂O₃ less than the FeO, but CaO more than MgO. And the rare earth elements of sandstones show an enrichment in light rare earth elements, a flat trending in heavy rare elements and a negative europium anomaly in most samples. However, there is a significant difference in the enrichment and loss of trace elements between samples. Related discriminations indicate that the source rocks of sandstones were carried and accumulated in short distance which mainly came from felsic rocks of the upper crust without experiencing deposition and recycling. Through the judgment combined with the geochemical characteristic, Dincksion diagram of sandstones and the study of regional tectonic setting, sandstones of Muling Formation have several provenances, and source region majorly was formed in the recycled orogeny and basement uplifted provenances under the tectonic background of active continental margin at the end of Indo-China Movement. Source rocks mostly came from felsic volcanic rocks and intrusive rocks during late Triassic to early-middle Jurassic, with a little probably from metamorphic of late Permian.

Key words: Laoheishan Basin, Muling Formation, geochemistry, provenance attribute, tectonic background, analysis of provenance

CLC Number:

XU Yinbo, LI Feng, ZHANG Jiaqiang, SUN Pingchang, BI Caiqin, TONG Lihua, LI Zhao. Geochemical Characteristics and Geological Implications of Sandstones in Muling Formation of Lower Cretaceous, Laoheishan Basin, Heilongjiang Province[J]. Geoscience, 2018, 32(04): 786-795.

Figures/Tables 15

References 29

[1]	黑龙江省地质矿产局. 黑龙江省区域地质志[M]. 北京: 地质出版社, 1993:192-216.
[2]	杨继权, 王秀琴, 刘殿生, 等. 黑龙江省大地构造单元划分及特征[J]. 世界地质, 2007, 26(4):426-434.
[3]	孙加鹏, 张兴洲, 杨宝俊. 张广才岭岩石圈结构及盆岭构造[J]. 长春科技大学学报, 1999, 29 (1):25-29.
[4]	国土资源部油气资源战略研究中心,吉林大学. 全国油页岩资源调查评价[M]. 北京: 中国大地出版社, 2010:149-151.
[5]	赵春荆. 吉黑东部构造格架及地壳演化[M]. 沈阳: 辽宁大学出版社, 1996:1-3.
[6]	李双林, 欧阳自远. 兴蒙造山带及邻区的构造格局与构造演化[J]. 海洋地质与第四纪地质, 1998, 18(3):45-54.
[7]	任纪舜, 牛宝贵, 刘志刚. 软碰撞、叠覆造山和多旋回缝合作用[J]. 地学前缘, 1999, 6(3):85-93.
[8]	孙德有, 吴福元, 张艳斌, 等. 西拉木伦河—长春—延吉板块缝合带的最后闭合时间——来自吉林大玉山花岗岩体的证据[J]. 吉林大学学报(地球科学版), 2004, 34(2):174-181.
[9]	李锦轶, 高立明, 孙桂华, 等. 内蒙古东部双井子中三叠世同碰撞壳源花岗岩的确定及其对西伯利亚与中朝古板块碰撞时限的约束[J]. 岩石学报, 2007, 23(3):565-582.
[10]	WU F Y, ZHAO G C, SUN D Y, et al. The Hulan group: its role in the evolution of the central Asian orogenic belt of NE China[J]. Journal of Asian Earth Sciences, 2007, 30(3):542-556. DOI URL
[11]	SONG Y, LIU Z, MENG Q, et al. Petrography and geochemistry characteristics of the lower Cretaceous Muling Formation from the Laoheishan Basin, Northeast China: implications for provenance and tectonic setting[J]. Mineralogy and Petrology, 2017, 111(3): 383-397. DOI URL
[12]	TAYLOR S R, MCLENNAN S M. The Continental Crust: Its Composition and Evolution[M]. Oxford: Blackwell, 1985: 57-72.
[13]	MCLENNAN S M, HEMMING S R, TAYLOR S R, et al. Early Proterozoic crustal evolution: Geochemical and Nd-Pb isotopic evi-dence from metasedimentary rocks, southwestern North America[J]. Geochimica et Cosmochimica Acta, 1995, 59(6): 1153-1177. DOI URL
[14]	MCLENNAN S M, TAYLOR S R, MCCULLOCH M T, et al. Geochemical and Nd/Sr isotopic composition of deep-sea turbidites: crustal evolution and plate tectonic associations[J]. Geochimica et Cosmochimica Acta, 1990, 54(7): 2015-2050. DOI URL
[15]	MCLENNAN S M, HEMMING S, MCDANIEL D K, et al. Geochemical approaches to sedimentation, provenance, and tectonics[J]. Special Paper of the Geological Society of America, 1993, 284: 21-40.
[16]	刘俊海, 杨香华, 于水, 等. 东海盆地丽水凹陷古新统沉积岩的稀土元素地球化学特征[J]. 现代地质, 2003, 17(4):421-427.
[17]	CULLERS R L, PODKOVYROV V N. Geochemistry of the Mesoproterozoic Lakhanda shales in southeastern Yakutia, Russia: implications for mineralogical and provenance control, and recycling[J]. Precambrian Research, 2000, 104(1): 77-93. DOI URL
[18]	FLOYD P A, LEVERIDGE B E. Tectonic environment of the Devonian Gramscatho Basin, South Comwall: Framework mode and geochemical evidence from turbiditic sandstone[J]. Journal of the Geology Society, 1987, 144(4): 531-542.
[19]	WRONKIEWICZ D J, CONDIE K C. Geochemistry of Archean shales from the Witwatersrand Supergroup, South Africa: Source-area weathering and provenance[J]. Geochimica et Cosmochimica Acta, 1987, 51(9):2401-2416. DOI URL
[20]	BHATIA M R, CROOK K A W. Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basin[J]. Contributions to Mineralogy and Petrology, 1986, 92(2): 181-193. DOI URL
[21]	DICKINSON W R, BEARD L S, BRAKENRIDGE G R, et al. Provenance of North American Phanerozoic sandstones in relation to tectonic setting[J]. Geological Society of America Bulletin, 1983, 94(2):222-235. DOI URL
[22]	DICKINSON W R, SUCZEK C A. Plate tectonics and sandstone compositions[J]. AAPG Bulletin, 1979, 63(12): 2164-2182.
[23]	陈安清, 陈洪德, 徐胜林, 等. 鄂尔多斯盆地北部晚古生代沉积充填与兴蒙造山带“软碰撞”的耦合[J]. 吉林大学学报(地球科学版), 2011, 41(4): 953-965.
[24]	李之彤, 赵春荆. 吉黑东部晚三叠世岩浆活动及其与板块构造的关系[J]. 中国地质科学院院报, 1988, 第18号: 21-32.
[25]	裴福萍, 许文良, 孟恩, 等. 古太平洋俯冲作用的开始: 来自吉黑东部早—中侏罗世火山岩的年代学及地球化学证据[J]. 矿物岩石地球化学通报, 2008, 27(s1): 268.
[26]	赵院冬, 迟效国, 车继英, 等. 延边—东宁地区晚三叠世花岗岩地球化学特征及其大地构造背景[J]. 吉林大学学报(地球科学版), 2009, 39(3):425-434.
[27]	任纪舜. 印支运动及其在中国大地构造演化中的意义[J]. 中国地质科学院院报, 1984, 第9号: 31-44.
[28]	杨宝俊, 张梅生, 王璞珺. 中国油气区地质-地球物理解析(上卷)[M]. 北京: 科学出版社, 2003: 40-126.
[29]	刘先文, 申宁华, 葛肖虹. 吉黑东部中生代两种机制的碰撞构造[J]. 长春地质学院学报, 1994, 24(4): 385-389.

样品	SiO₂	Al₂O₃	Fe₂O₃	FeO	CaO	MgO	K₂O	Na₂O	TiO₂	P₂O₅	MnO	烧失量
N1	53.56	10.62	1.22	1.88	12.78	0.84	2.90	2.00	0.35	0.04	0.41	13.04
N2	65.45	14.28	2.94	2.45	1.41	1.39	3.65	2.72	0.37	0.07	0.08	5.11
N3	69.80	15.28	0.11	1.96	1.07	0.94	3.80	2.82	0.63	0.10	0.03	2.98
N4	70.01	15.15	1.03	1.15	1.16	0.94	3.85	2.89	0.49	0.09	0.03	2.72
N5	69.19	15.47	2.51	0.67	1.92	2.81	0.47	1.08	0.16	0.05	0.01	5.48
N6	72.14	14.50	0.53	1.23	0.95	0.77	3.78	3.00	0.49	0.10	0.03	2.26
N7	66.99	18.06	1.26	0.74	1.21	1.25	3.41	2.54	0.51	0.10	0.02	3.85
N8	66.81	17.03	1.06	1.67	0.93	1.00	3.43	2.55	0.72	0.12	0.04	4.38
N9	71.79	15.23	0.53	1.23	0.52	0.50	3.84	2.15	0.46	0.04	0.03	3.22
N10	59.54	22.09	0.97	1.47	0.59	0.83	2.40	1.12	0.83	0.02	0.01	9.86
N11	67.05	15.52	0.85	1.72	1.10	0.78	2.96	1.98	0.55	0.07	0.02	7.27
N12	64.42	18.25	2.06	0.90	1.83	1.91	3.18	2.69	0.53	0.20	0.02	3.77
N13	63.31	16.18	1.81	2.94	2.05	1.37	3.12	2.47	0.65	0.14	0.07	5.56
N14	60.95	22.15	1.51	1.72	0.61	0.78	2.54	1.27	0.85	0.06	0.03	7.06
N15	60.20	16.24	1.98	5.79	0.93	1.19	2.00	0.23	0.85	0.03	0.07	10.23

样品	SiO₂	Al₂O₃	Fe₂O₃	FeO	CaO	MgO	K₂O	Na₂O	TiO₂	P₂O₅	MnO	烧失量
N1	53.56	10.62	1.22	1.88	12.78	0.84	2.90	2.00	0.35	0.04	0.41	13.04
N2	65.45	14.28	2.94	2.45	1.41	1.39	3.65	2.72	0.37	0.07	0.08	5.11
N3	69.80	15.28	0.11	1.96	1.07	0.94	3.80	2.82	0.63	0.10	0.03	2.98
N4	70.01	15.15	1.03	1.15	1.16	0.94	3.85	2.89	0.49	0.09	0.03	2.72
N5	69.19	15.47	2.51	0.67	1.92	2.81	0.47	1.08	0.16	0.05	0.01	5.48
N6	72.14	14.50	0.53	1.23	0.95	0.77	3.78	3.00	0.49	0.10	0.03	2.26
N7	66.99	18.06	1.26	0.74	1.21	1.25	3.41	2.54	0.51	0.10	0.02	3.85
N8	66.81	17.03	1.06	1.67	0.93	1.00	3.43	2.55	0.72	0.12	0.04	4.38
N9	71.79	15.23	0.53	1.23	0.52	0.50	3.84	2.15	0.46	0.04	0.03	3.22
N10	59.54	22.09	0.97	1.47	0.59	0.83	2.40	1.12	0.83	0.02	0.01	9.86
N11	67.05	15.52	0.85	1.72	1.10	0.78	2.96	1.98	0.55	0.07	0.02	7.27
N12	64.42	18.25	2.06	0.90	1.83	1.91	3.18	2.69	0.53	0.20	0.02	3.77
N13	63.31	16.18	1.81	2.94	2.05	1.37	3.12	2.47	0.65	0.14	0.07	5.56
N14	60.95	22.15	1.51	1.72	0.61	0.78	2.54	1.27	0.85	0.06	0.03	7.06
N15	60.20	16.24	1.98	5.79	0.93	1.19	2.00	0.23	0.85	0.03	0.07	10.23

样品	Li	B		Sc		V		Cr		Co		Ni		Cu		Zn	Ga		Rb		Sr		Zr		Nb
N1	12.14	11.08		6.38		46.76		21.22		5.03		9.81		3.86		27.44	13.53		97.68		300.00		97.87		6.15
N2	15.06	19.86		4.80		34.98		17.01		9.31		10.03		4.81		44.77	14.68		43.38		207.50		111.60		5.99
N3	11.12	21.22		5.15		55.05		32.08		4.83		9.34		5.39		28.75	16.42		75.46		265.50		144.30		8.50
N4	17.00	13.21		5.90		44.32		30.87		3.48		7.11		5.78		44.12	18.56		110.50		340.30		56.25		6.60
N5	34.50	10.78		3.29		10.40		12.22		1.84		7.19		4.84		47.39	19.17		14.76		582.60		77.74		13.14
N6	9.71	24.36		3.45		45.86		30.66		2.93		7.97		7.82		47.22	14.52		84.33		249.20		124.40		7.50
N7	15.37	20.36		5.72		46.84		29.63		2.69		7.10		6.82		38.73	20.89		81.09		352.80		141.20		11.50
N8	35.13	25.23		9.01		72.20		47.03		17.13		31.77		16.55		75.37	21.93		106.60		288.70		117.70		12.27
N9	38.42	15.73		9.29		52.21		23.18		3.35		4.63		6.20		43.50	17.35		112.00		90.22		64.76		7.69
N10	125.70	40.35		10.17		60.72		35.72		3.31		8.44		13.78		43.14	25.74		102.40		198.30		90.70		10.99
N11	49.38	39.18		3.68		68.30		40.14		5.64		9.55		11.53		80.82	19.64		94.48		228.60		120.30		9.22
N12	29.99	30.86		3.05		37.98		11.77		14.44		24.06		67.88		137.80	23.05		20.74		523.60		151.50		5.50
N13	23.51	25.34		8.71		59.36		43.29		7.30		15.71		14.01		78.40	20.56		100.40		407.70		106.00		10.70
N14	106.40	75.54		6.22		107.30		44.26		6.09		13.40		18.97		59.52	22.96		51.83		113.30		208.80		13.07
N15	83.65	53.64		15.70		113.50		111.40		21.35		22.05		15.65		102.40	23.55		41.61		72.63		226.70		8.18
样品	Mo	Cs		Hf		Th		U		La		Ce		Pr		Nd	Sm		Eu		Gd		Tb		Dy
N1	0.43	2.56		3.01		6.40		3.85		24.25		44.80		5.09		19.23	4.00		1.01		4.29		0.67		4.43
N2	0.54	2.21		3.24		4.17		2.35		11.46		23.33		2.84		11.03	2.17		0.55		2.06		0.28		2.04
N3	1.00	2.47		4.28		20.24		4.24		15.28		29.93		3.54		13.32	2.57		0.70		2.39		0.32		2.09
N4	0.61	3.03		2.07		5.84		1.68		16.75		32.30		3.84		14.18	2.71		0.73		2.36		0.30		1.82
N5	1.90	1.09		3.18		9.92		3.09		29.18		52.77		5.88		19.19	3.23		0.46		2.56		0.32		1.93
N6	0.52	2.55		3.73		4.35		2.35		13.17		25.24		3.17		11.90	2.23		0.63		1.93		0.26		1.63
N7	2.74	2.23		4.82		7.84		2.85		21.51		41.48		4.76		17.61	3.35		0.81		3.02		0.43		2.69
N8	1.12	6.14		4.17		11.72		4.40		27.46		53.62		6.94		26.62	5.22		1.16		4.68		0.63		3.75
N9	0.45	2.92		2.58		11.62		3.25		17.47		35.30		4.22		15.69	3.24		0.78		3.02		0.44		2.88
N10	0.26	11.50		3.08		13.53		2.54		18.79		32.89		4.18		15.01	2.91		0.74		2.67		0.40		2.63
N11	1.49	4.82		3.19		9.26		3.57		26.59		54.14		6.40		23.82	4.69		1.18		4.25		0.59		3.57
N12	5.01	1.04		4.46		4.24		2.09		14.03		32.82		3.65		14.06	2.68		0.82		2.19		0.25		1.35
N13	0.34	4.25		3.52		9.86		4.47		31.30		59.42		7.56		29.37	5.72		1.60		5.23		0.74		4.31
N14	0.58	6.53		6.45		8.77		3.14		16.02		35.44		4.25		16.45	3.50		0.75		3.44		0.54		3.57
N15	0.26	4.85		6.77		5.96		2.12		22.65		50.50		6.52		26.75	6.23		1.44		6.21		1.00		6.77
样品	Ho		Er		Tm		Yb		Lu		Y		Th/U		La_N/Yb_N			δEu		δCe		LREE/HREE		∑REE
N1	0.92		2.68		0.38		2.35		0.35		29.75		1.66		6.95			0.75		0.97		6.12		144.19
N2	0.44		1.38		0.22		1.55		0.22		11.35		1.77		4.97			0.79		0.98		6.27		70.93
N3	0.43		1.28		0.20		1.28		0.19		10.39		4.77		8.04			0.87		0.98		7.99		83.91
N4	0.36		1.06		0.16		1.03		0.15		9.07		3.47		10.99			0.89		0.97		9.74		86.83
N5	0.35		1.03		0.15		1.01		0.14		10.08		3.21		19.56			0.49		0.97		14.82		128.26
N6	0.31		0.96		0.15		0.94		0.14		6.94		1.85		9.48			0.93		0.94		8.93		69.58
N7	0.53		1.60		0.24		1.62		0.24		13.16		2.75		8.94			0.78		0.99		8.62		113.06
N8	0.74		2.27		0.35		2.12		0.32		18.42		2.66		8.72			0.72		0.93		8.14		154.32
N9	0.59		1.72		0.27		1.88		0.27		14.36		3.57		6.27			0.76		0.99		6.92		102.13
N10	0.58		1.91		0.30		2.14		0.34		16.84		5.33		5.91			0.82		0.89		6.79		102.33
N11	0.71		2.10		0.32		2.08		0.31		18.01		2.59		8.61			0.81		1.00		8.39		148.75
N12	0.24		0.68		0.09		0.55		0.07		6.10		2.03		17.06			1.04		1.10		12.52		79.59
N13	0.83		2.39		0.35		2.16		0.31		21.47		2.21		9.78			0.89		0.93		8.28		172.75
N14	0.76		2.35		0.39		2.72		0.42		15.24		2.79		3.98			0.66		1.03		5.39		105.83
N15	1.46		4.53		0.70		4.73		0.71		32.51		2.80		3.23			0.71		1.00		4.37		172.69

样品	Li	B		Sc		V		Cr		Co		Ni		Cu		Zn	Ga		Rb		Sr		Zr		Nb
N1	12.14	11.08		6.38		46.76		21.22		5.03		9.81		3.86		27.44	13.53		97.68		300.00		97.87		6.15
N2	15.06	19.86		4.80		34.98		17.01		9.31		10.03		4.81		44.77	14.68		43.38		207.50		111.60		5.99
N3	11.12	21.22		5.15		55.05		32.08		4.83		9.34		5.39		28.75	16.42		75.46		265.50		144.30		8.50
N4	17.00	13.21		5.90		44.32		30.87		3.48		7.11		5.78		44.12	18.56		110.50		340.30		56.25		6.60
N5	34.50	10.78		3.29		10.40		12.22		1.84		7.19		4.84		47.39	19.17		14.76		582.60		77.74		13.14
N6	9.71	24.36		3.45		45.86		30.66		2.93		7.97		7.82		47.22	14.52		84.33		249.20		124.40		7.50
N7	15.37	20.36		5.72		46.84		29.63		2.69		7.10		6.82		38.73	20.89		81.09		352.80		141.20		11.50
N8	35.13	25.23		9.01		72.20		47.03		17.13		31.77		16.55		75.37	21.93		106.60		288.70		117.70		12.27
N9	38.42	15.73		9.29		52.21		23.18		3.35		4.63		6.20		43.50	17.35		112.00		90.22		64.76		7.69
N10	125.70	40.35		10.17		60.72		35.72		3.31		8.44		13.78		43.14	25.74		102.40		198.30		90.70		10.99
N11	49.38	39.18		3.68		68.30		40.14		5.64		9.55		11.53		80.82	19.64		94.48		228.60		120.30		9.22
N12	29.99	30.86		3.05		37.98		11.77		14.44		24.06		67.88		137.80	23.05		20.74		523.60		151.50		5.50
N13	23.51	25.34		8.71		59.36		43.29		7.30		15.71		14.01		78.40	20.56		100.40		407.70		106.00		10.70
N14	106.40	75.54		6.22		107.30		44.26		6.09		13.40		18.97		59.52	22.96		51.83		113.30		208.80		13.07
N15	83.65	53.64		15.70		113.50		111.40		21.35		22.05		15.65		102.40	23.55		41.61		72.63		226.70		8.18
样品	Mo	Cs		Hf		Th		U		La		Ce		Pr		Nd	Sm		Eu		Gd		Tb		Dy
N1	0.43	2.56		3.01		6.40		3.85		24.25		44.80		5.09		19.23	4.00		1.01		4.29		0.67		4.43
N2	0.54	2.21		3.24		4.17		2.35		11.46		23.33		2.84		11.03	2.17		0.55		2.06		0.28		2.04
N3	1.00	2.47		4.28		20.24		4.24		15.28		29.93		3.54		13.32	2.57		0.70		2.39		0.32		2.09
N4	0.61	3.03		2.07		5.84		1.68		16.75		32.30		3.84		14.18	2.71		0.73		2.36		0.30		1.82
N5	1.90	1.09		3.18		9.92		3.09		29.18		52.77		5.88		19.19	3.23		0.46		2.56		0.32		1.93
N6	0.52	2.55		3.73		4.35		2.35		13.17		25.24		3.17		11.90	2.23		0.63		1.93		0.26		1.63
N7	2.74	2.23		4.82		7.84		2.85		21.51		41.48		4.76		17.61	3.35		0.81		3.02		0.43		2.69
N8	1.12	6.14		4.17		11.72		4.40		27.46		53.62		6.94		26.62	5.22		1.16		4.68		0.63		3.75
N9	0.45	2.92		2.58		11.62		3.25		17.47		35.30		4.22		15.69	3.24		0.78		3.02		0.44		2.88
N10	0.26	11.50		3.08		13.53		2.54		18.79		32.89		4.18		15.01	2.91		0.74		2.67		0.40		2.63
N11	1.49	4.82		3.19		9.26		3.57		26.59		54.14		6.40		23.82	4.69		1.18		4.25		0.59		3.57
N12	5.01	1.04		4.46		4.24		2.09		14.03		32.82		3.65		14.06	2.68		0.82		2.19		0.25		1.35
N13	0.34	4.25		3.52		9.86		4.47		31.30		59.42		7.56		29.37	5.72		1.60		5.23		0.74		4.31
N14	0.58	6.53		6.45		8.77		3.14		16.02		35.44		4.25		16.45	3.50		0.75		3.44		0.54		3.57
N15	0.26	4.85		6.77		5.96		2.12		22.65		50.50		6.52		26.75	6.23		1.44		6.21		1.00		6.77
样品	Ho		Er		Tm		Yb		Lu		Y		Th/U		La_N/Yb_N			δEu		δCe		LREE/HREE		∑REE
N1	0.92		2.68		0.38		2.35		0.35		29.75		1.66		6.95			0.75		0.97		6.12		144.19
N2	0.44		1.38		0.22		1.55		0.22		11.35		1.77		4.97			0.79		0.98		6.27		70.93
N3	0.43		1.28		0.20		1.28		0.19		10.39		4.77		8.04			0.87		0.98		7.99		83.91
N4	0.36		1.06		0.16		1.03		0.15		9.07		3.47		10.99			0.89		0.97		9.74		86.83
N5	0.35		1.03		0.15		1.01		0.14		10.08		3.21		19.56			0.49		0.97		14.82		128.26
N6	0.31		0.96		0.15		0.94		0.14		6.94		1.85		9.48			0.93		0.94		8.93		69.58
N7	0.53		1.60		0.24		1.62		0.24		13.16		2.75		8.94			0.78		0.99		8.62		113.06
N8	0.74		2.27		0.35		2.12		0.32		18.42		2.66		8.72			0.72		0.93		8.14		154.32
N9	0.59		1.72		0.27		1.88		0.27		14.36		3.57		6.27			0.76		0.99		6.92		102.13
N10	0.58		1.91		0.30		2.14		0.34		16.84		5.33		5.91			0.82		0.89		6.79		102.33
N11	0.71		2.10		0.32		2.08		0.31		18.01		2.59		8.61			0.81		1.00		8.39		148.75
N12	0.24		0.68		0.09		0.55		0.07		6.10		2.03		17.06			1.04		1.10		12.52		79.59
N13	0.83		2.39		0.35		2.16		0.31		21.47		2.21		9.78			0.89		0.93		8.28		172.75
N14	0.76		2.35		0.39		2.72		0.42		15.24		2.79		3.98			0.66		1.03		5.39		105.83
N15	1.46		4.53		0.70		4.73		0.71		32.51		2.80		3.23			0.71		1.00		4.37		172.69