ORIGIN OF QUATERNARY MUDDY GRAVEL DEPOSITS IN THE LUSHAN AREA

LIU Zong-xiu; ZHAO Zhi-zhong; TIAN Jiao-rong; WANG Min; LI Ming-ze

Volume 13 Issue 4

Dec. 2007

Turn off MathJax

Article Contents

Abstract

References

Article Navigation > Journal of Geomechanics > 2007 > 13(4): 322-332, 314

DING Ti-ping, 2000. ISOTOPIC CONSTRAINTS ON THE FORMATION DEPTH OF ULTRAHIGH PRESSURE METAMORPHIC ROCKS IN THE DABIE REGION. Journal of Geomechanics, 6 (3): 39-44.

Citation:

LIU Zong-xiu, ZHAO Zhi-zhong, TIAN Jiao-rong, et al., 2007. ORIGIN OF QUATERNARY MUDDY GRAVEL DEPOSITS IN THE LUSHAN AREA. Journal of Geomechanics, 13 (4): 322-332, 314.

DING Ti-ping, 2000. ISOTOPIC CONSTRAINTS ON THE FORMATION DEPTH OF ULTRAHIGH PRESSURE METAMORPHIC ROCKS IN THE DABIE REGION. Journal of Geomechanics, 6 (3): 39-44.

Citation:

LIU Zong-xiu, ZHAO Zhi-zhong, TIAN Jiao-rong, et al., 2007. ORIGIN OF QUATERNARY MUDDY GRAVEL DEPOSITS IN THE LUSHAN AREA. Journal of Geomechanics, 13 (4): 322-332, 314.

PDF( 527 KB)

ORIGIN OF QUATERNARY MUDDY GRAVEL DEPOSITS IN THE LUSHAN AREA

1.
Institute of Geomechanics, Chinese Academy of Geological Science, Beijing 100081, China
2.
Chinese Research Center of National Geopark, Beijing 100081, China
3.
Lushan Administrative Bureau, Jiujiang 332900, Jiangxi, China

More Information

Abstract

Abstract

The gravel fabric characteristics of Quaternary muddy gravel deposits in the Lushan area indicate the following:the lithology of gravels is almost consistent with that of bedrocks in the mountains; the isometric sphere diameter of gravels is small, the weighted average diameter of gravels is lower than the median diameter of gravel; the gravels are poorly sorted with a sorting coefficient of >1;the values are relatively lower, averaging -0.66;the F values are higher, being 22.75%-37.75%;the ratios of F/φ range from 2.75 to 4.75;the φ values are lower and concentrated, ranging from 22.75 to 37.75%, and the gravels are mainly angular and subangular.Both the a-axis and ab-plane dip towards the downstream, the dip angles of the a-axis are low and concentrated, being 7-8°, the ab-plane dips at 7～21°, and the a-axis has more preferred dip of fabrics than the ab-plane; the peak of the grain-size frequency distribution curve of deposits in the Lushan area is in the range of 4 and 5φ; The quartz sand grains are subangular and have well-developed conchoidal fractures, parallel striations, upturned cleavage flakes, "V"-shaped holes and siliceous deposits.The above-mentioned sedimentary characteristics indicate that the Quaternary muddy gravel deposits in the Lushan area should be till and glaciofluvial deposits rather than fluvial deposits or mudflows.
- Lushan Mountain,
- muddy gravel,
- fabric characteristics,
- till

FullText(HTML)

References(32)

References

[1]	李四光. 冰期之庐山[M]. 前中央研究院地质研究所专刊乙种, 第2号, 1947.
[2]	Lee J S.Data relating to the study of the problem of glaciation in the lower Yangtze valley[J].Bull.Geol.Soc.China.1934, 8(3):395～ 422. http://cn.bing.com/academic/profile?id=e5d4dd7d520816b393026b54e977dd2f&encoded=0&v=paper_preview&mkt=zh-cn
[3]	何培元, 潘建英. 庐山高垄-白石嘴砾石层的组构特征及其成因探讨[J]. 第四纪冰川与第四纪地质文集(第三集). 北京: 地质出版社, 1992: 354～ 370.
[4]	何培元, 段万倜, 邢历生, 等.庐山第四纪冰期与环境[M].北京:地震出版社, 1992:34～ 44.
[5]	孙殿卿, 杨怀仁.大冰期时期中国的冰川遗迹[J].地质学报, 1961, (3/4):233～ 244. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000377282
[6]	赵良政.庐山东南麓冰川作用表皮构造特征及其意义[J].武汉地质学院学报(地球科学版), 1985, 10 (4):71 ～ 75. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=DQKX198504011&dbname=CJFD&dbcode=CJFQ
[7]	黄培华.五十年来中国东部第四纪冰川问题的研究及其争论[J].冰川冻土, 1983, (2):1～ 8. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000001049240
[8]	黄培华.中国第四纪气候演变与庐山"冰川遗迹"问题[J].冰川冻土, 1982, (3):1～ 14. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000001049200
[9]	施雅风.庐山真的有第四纪冰川吗?[J].自然辩证法通讯, 1981, (2):41～ 45. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ZRBT198102007&dbname=CJFD&dbcode=CJFQ
[10]	姚檀栋, 李吉均.庐山地区"冰斗"、"U谷"及"泥砾"成因之辨析[J].冰川冻土, 1982, (4):27～ 42. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000001049214
[11]	爱·德比希尔.庐山的困境:长江以南的更新世冰川作用[J].冰川冻土, 1982, (4):1～ 26. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=BCDT198204000&dbname=CJFD&dbcode=CJFQ
[12]	邓晓峰.庐山羊角岭附近混杂堆积的组构特征及其成因[J].冰川冻土, 1984, (3):87～ 89. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000001049346
[13]	陈怀录, 艾南山.庐山地区混杂堆积物砾向计算初步结果[J].兰州大学学报(自然科学版), 1983, (2):128～ 129. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000002074168
[14]	邓养鑫.庐山羊角岭附近"泥砾"成因的泥石流解释[J].冰川冻土, 1983, (1):33～ 46. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000001049231
[15]	施雅风, 邓养鑫.庐山山麓第四纪泥石流堆积的确证———以庐山西北麓羊角岭为例[J].科学通报, 1982, (20): 1253～ 1258. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=KXTB198220012&dbname=CJFD&dbcode=CJFQ
[16]	谢又予, 吴淑安.九江-庐山地区第四纪沉积环境的初步探讨[J].地理集刊, 1981, 13号:106～ 132.
[17]	彭汉学.庐山红色泥砾泥石流成因商榷[J].冰川冻土, 1990, 12 (1):87～ 90. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000001049687
[18]	Dreimanis A, Vagners U.The dependence of the composition of till upon the rule of bimodal distribution[J].Etudes sur le Quaternaire dans le Monde, 1969, 2.
[19]	Mills H.Textural characteristics of drift from some representative Cordilleran glaciers[J].Geo.Soc.Am.Bull, 1971, 88.
[20]	Slatt F.Texture of ice cores deposits from ten Alaska valley glaciers[J].J.S.P., 1971, 41 (3).
[21]	马正海.天山和青藏高原等地冰碛物粒度组成的初步分析[J].冰川冻土, 1980, 2 (增刊):80～ 83. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000001049087
[22]	武安斌.兰州许家滩-雁滩河漫滩砾石的沉积组构分析[J].兰州大学学报(自然科学版), 1977, (3):119～ 125. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000002073759
[23]	周秉根, 李典友.黄山不同类型砾石特性及成因分析[J].安徽师范大学学报(自然科学版), 2000, (1):57～ 60. doi: 10.3969/j.issn.1001-2443.2000.01.018
[24]	张志良, 何培元.太行山东麓现代泥石流特征[J].地质论评, 1981, 27 (6):514～ 519. doi: 10.3321/j.issn:0371-5736.1981.06.006
[25]	武安斌.疏勒南山岗纳楼5号冰川现代冰碛物的沉积组构特征[J].兰州大学学报(自然科学版), 1980 (3):119 ～ 126. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000002073929
[26]	王爱军, 高抒, 杨旸.浙江朱家尖岛砾石海滩沉积物分布及形态特征[J].南京大学学报(自然科学版), 2004, (6):747～ 759. doi: 10.3321/j.issn:0469-5097.2004.06.011
[27]	朱大岗, 赵希涛, 孟宪刚, 等.念青唐古拉山主峰地区第四纪砾石层砾组分析[J].地质力学学报, 2002, (4): 323～ 332. doi: 10.3969/j.issn.1006-6616.2002.04.006
[28]	邓晓峰, 王存年.天山博格达峰地区冰碛物和冰缘沉积物的砾石组构特征[J].冰川冻土, 1983, (3):217～ 226. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000001049281
[29]	第四纪冰川考察队. 四川西昌螺髻山地区第四纪砾石层的砾组分析[C]. 中国第四纪冰川地质文集. 北京: 地质出版社, 1977: 191～ 228.
[30]	第四纪冰川考察队. 关于西昌砾石层[C]. 中国第四纪冰川地质文集. 北京: 地质出版社, 1977: 155～ 163.
[31]	施雅风, 崔之久, 李吉均, 等.中国东部第四纪冰川与环境问题[M].北京:科学出版社, 1989:225～ 248.
[32]	谢国刚, 冯晔, 马振兴.庐山地区第四纪岩石地层单位划分[J].江西地质, 1994, (4):272～ 280. http://d.old.wanfangdata.com.cn/Conference/53775

Relative Articles

	TANG Haibing, WU Jianjun, ZHANG Chunshan, YANG Weimin, QU Jingkai, MA Siqi, XU Chuancheng. 2024: Debris flow hazard analysis before and after improvement of Hanjia gully control engineering at the source area of the Fujiang River. Journal of Geomechanics, 30(4): 659-672. doi: 10.12090/j.issn.1006-6616.2023097
	GU Zhenkui, YAO Xin, LI Lingjing, TAO Tao. 2023: Applying stream power gradient in the investigation on spatial susceptibility of debris flow: A case of the Jinsha River Basin, China. Journal of Geomechanics, 29(1): 87-98. doi: 10.12090/j.issn.1006-6616.2022022
	ZHANG Xianzheng, TIE Yongbo, LI Guanghui, YANG Chang, LU Jiayan, LU Tuo. 2022: Characteristics and risk assessment of debris flows in the Wandong catchment after the M_S 6.8 Luding earthquake. Journal of Geomechanics, 28(6): 1035-1045. doi: 10.12090/j.issn.1006-6616.20222827
	ZHANG Haowei, LIU Fuzhen, WANG Junchao, ZHANG Jiajia. 2022: Hazard assessment of debris flows in Kongpo Gyamda, Tibet based on FLO-2D numerical simulation. Journal of Geomechanics, 28(2): 306-318. doi: 10.12090/j.issn.1006-6616.2021117
	MA Siqi, YANG Weimin, ZHANG Chunshan, QU Jingkai, WAN Feipeng, TANG Haibing. 2022: Provenance characteristics and risk analysis of debris flows in Siergou, Lanzhou City. Journal of Geomechanics, 28(6): 1059-1070. doi: 10.12090/j.issn.1006-6616.20222829
	LI Yihao, DU Xingxing, LI Tianxiu. 2022: Characterization of the Holocene extensional structures in the Wuwei Basin, northeastern margin of the Tibetan Plateau, and their formation mechanism. Journal of Geomechanics, 28(3): 353-366. doi: 10.12090/j.issn.1006-6616.2021151
	WANG Zhaobo, WANG Jiangyue, HE Lelong, ZHANG Jian, ZHAO Xiangyang, LI Baojie. 2021: Characteristics and evolution process of the ridge-groove sequence of the Jiulongtan glacial accumulation in Mengshan, Shandong: with the discussion on the difference of accumulation sequence of glacier and debris flow. Journal of Geomechanics, 27(1): 105-116. doi: 10.12090/j.issn.1006-6616.2021.27.01.011
	LIU Yu-ping, LIANG Hong, CHENG Fi-fi. 2016: APPLICATION OF HIGH RESOLUTION AIRBORNE LIDAR IN XIAOJIANG ACTIVE TECTONICS AND GEOLOGICAL DISASTER STUDY. Journal of Geomechanics, 22(3): 747-759.
	ZHANG Rui-duan, GUO Chang-bao, ZHANG Yong-shuang, FU Xiao-xiao. 2014: DEVELOPMENT CHARACTERISTICS AND PREVENTION SUGGESTIONS OF THE LEPA DEBRIS FLOW IN THE ANNING RIVER FAULT ZONE. Journal of Geomechanics, 20(2): 132-139.
	SHI Ling, WANG Tao, XIN Peng. 2013: DEVELOPMENT CHARACTERISTICS OF THE GEO-HARZARDS IN BAOJI CITY, SHAANXI PROVINCE. Journal of Geomechanics, 19(4): 351-363.
	ZHAO Zhi-li, WANG Yong, CHI Zhen-qing, GUAN You-yi, YAO Pei-yi. 2011: ENVIROMENTAL CHANGES RECORDED BY POLLEN SINCE MID TO LATE HOLOCENE IN HUITENGXILE LAKE, LNNER MONGOLIA. Journal of Geomechanics, 17(1): 103-110.
	XIONG Tan-yu, YAO Xin, ZHANG Yong-shuang. 2010: A REVIEW ON STUDY OF ACTIVITY OF XIANSHUIHE FAULT ZONE SINCE THE HOLOCENE. Journal of Geomechanics, 16(2): 176-188.
	WANG Xian-li, QU Yong-xin, JIANG Liang-wen, ZHANG Yong-shuang. 2007: ENGINEERING PROPERTIES OF EARLY HOLOCENE SOFT CLAY ON THE EAST BANK OF ERHAI LAKE. Journal of Geomechanics, 13(3): 261-269.
	DING Ji-xin, YANG Zhi-fa, SHANG Yan-jun. 2006: CAUSE ANALYSIS AND QUANTITATIVE ZONATION OF MUDFLOW HAZARDS ALONG THE RAWU-LUNANG SECTION, SICHUAN-TIBET HIGHWAY. Journal of Geomechanics, 12(2): 203-210,226.
	WANG Yan, YE Qing-pei, QIAO Yan-song. 2006: PALYNOLOGICAL RECORDS OF THE HOLOCENE ENVIRONMENTAL CHANGES IN ZHENGLAN QI, INNER MONGOLIA. Journal of Geomechanics, 12(3): 324-328.
	ZHANG Chun-shan, ZHANG Ye-cheng, ZHANG Li-hai. 2004: DANGER ASSESSMENT OF COLLAPSES,LANDSLIDES AND DEBRIS FLOWS OF GEOLOGICAL HAZARDS IN CHINA. Journal of Geomechanics, 10(1): 27-32.
	CUI Zhi-jiu, TANG Yuan-xin, LI Jian-jiang, LIU Hong-yan, LIU Geng-nian. 2003: INFORMATION OF HOLOCENE ENVIRONMENTAL CHANGE FROM LACUSTRIAN DEPOSITS OF THE FOYECHI LAKE SECTION,TAIBAI MOUNTAIN. Journal of Geomechanics, 9(4): 330-336.
	TIAN Xiao-xian. 2000: STUDIES ON THE FEATURES OF THE HOLBAOJINAO QUARTERNARY SALT LAKE IN MID-NORTH ERDOS BASIN. Journal of Geomechanics, 6(1): 84-89,94.
	LIU Xi-lin. 2000: DEBRIS FLOW RISK ZONATION IN ZHAOTONG COUNTY OF YUNNAN PROVINCE,CHINA. Journal of Geomechanics, 6(4): 37-42.
	Lao Xiong. 1995: ON THE FORMATION OF YARLUNG ZANGBO RIVER FAULT ZONE. Journal of Geomechanics, 1(1): 53-59.

Supplements(0)

Cited By

Cited by

Periodical cited type(2)

1.	赵聪，梁京涛，铁永波，马晓波，张肃，龚凌枫. 西藏雅鲁藏布江峡谷特大巨型泥石流活动与泥沙输移特征研究. 中国地质灾害与防治学报. 2024(04): 45-55 .
2.	张国忠，李德华，廖俊雄，周沁铃. 得荣县泥石流的诱发降雨阈值分析. 农业灾害研究. 2024(10): 224-226+323 .

Other cited types(2)

Proportional views

Proportional views

Figures(5) / Tables(4)

Get Citation

PDF

XML

Article Metrics

Article views (298) PDF downloads(7)

ORIGIN OF QUATERNARY MUDDY GRAVEL DEPOSITS IN THE LUSHAN AREA