帕米尔东北缘新生代隆升活动：来自奥依塔格剖面砾石统计的证据

廖林; 陈汉林; 程晓敢; 林秀斌; 赵学钦; 姚琪; 周玉彬; 白琰

doi:10.3799/dqkx.2012.088

帕米尔东北缘新生代隆升活动：来自奥依塔格剖面砾石统计的证据

doi: 10.3799/dqkx.2012.088

廖林^{1, 2,},
陈汉林^{1, 2},
程晓敢^{1, 2},
林秀斌^{1, 2},
赵学钦^{1, 2},
姚琪³,
周玉彬⁴,
白琰⁵

1.
浙江大学地球科学系，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.
中国地震局地质研究所，北京 100029
4.
中石油西南油气田公司川西北气矿，四川江油 621709
5.
延长油田股份有限公司，陕西延安 717600

基金项目:

国家自然科学基金 40972138

国家自然科学基金 41072154

详细信息

作者简介:
廖林(1978-)，男，工程师，博士，主要从事造山带与盆地构造分析、盆地动力学方面的研究.E-mail: geollin@zju.edu.cn

中图分类号: P534
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出版历程
- 收稿日期: 2012-02-28
- 网络出版日期: 2021-10-13
- 刊出日期: 2012-07-15

Cenozoic Uplift of the Northeastern Pamir: Evidence from the Gravel Counting Results of the Oytag Section

LIAO Lin^{1, 2
,},
CHEN Han-lin^{1, 2},
CHENG Xiao-gan^{1, 2},
LIN Xiu-bin^{1, 2},
ZHAO Xue-qin^{1, 2},
YAO Qi³,
ZHOU Yu-bin⁴,
BAI Yan⁵

1.
Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China
2.
Structural Research Center of Oil and Gas Bearing Basin of Ministry of Education, Hangzhou 310027, China
3.
Institute of Geology, China Earthquake Administration, Beijing 100029, China
4.
Southwest Oil and Gas Field Company, CNPC, Jiangyou 621709, China
5.
Yanchang Oil Field Co. Ltd., Yan'an 717600, China

摘要

摘要: 砾岩相通常作为构造事件的标志，对探讨造山带隆升过程有着重要的意义.选取位于帕米尔构造带东北缘的奥依塔格剖面开展砾石统计分析.新生代不同时期砾石的统计结果显示，奥依塔格剖面砾石成分主要为火成岩和变质岩，这与帕米尔造山带岩性相符.其中，花岗岩砾石作为特征组分首次出现在上新统阿图什组底部.砾石主要为巨砾，且以长短轴比值为1~2的近圆状为主；砾石的磨圆度中等，绝大部分为次磨圆-次棱角状；分选中等-差.结合砾石所处地层的沉积环境和热年代学记录，认为帕米尔东北缘新生代可能存在3期构造隆升事件，包括渐新-中新世克孜洛依组沉积早期、中新世中期(安居安组中-上段和帕卡布拉克组下段沉积时期)和上新世以来(阿图什组下段沉积以来).
- 帕米尔东北缘 /
- 新生代 /
- 隆升 /
- 砾石统计 /
- 奥依塔格 /
- 沉积学 /
- 构造
Abstract: The study of gravel-facies, an important sedimentary indicator of tectonic event could facilitate the understanding of the evolution of the uplift in orogen. In this paper, the Cenozoic gravels in Oytag section located in the piedmont of northeastern Pamir, has been chosen to conduct gravel counting. The results show that gravels in Cenozoic are mainly igneous and metamorphic, indicating that they came from Pamir area. As the first occurrence of new gravel types, the granite gravel emerges at the bottom of Atushi Formation of Pliocene. The gravels are mainly of giant-size, sub-rounded and sub-angular, moderated and middling to bad sorted, with a ratio of the length of maximum axis to the minimum axis ranging from 1 to 2. Combined with Cenozoic depositing environment and thermochronology records, following uplifting periods have been identified in northeastern Pamir as Late Oligocene to Early Miocene, Mid Miocene and since Early Pliocene.
- northeastern Pamir /
- Cenozoic /
- uplift /
- gravel counting /
- Oystag /
- sedimentology /
- tectonics

HTML全文

图 1 帕米尔东北缘地质简图(据Sobel and Dumitru, 1997；Yin et al., 2002；廖林，2010修改)

F1.帕米尔东北缘主冲断裂；F2.乌泊尔断裂；F3.库姆塔格断裂；JJS.金沙缝合线；ATF.阿尔金断裂；EKL.东昆仑断裂；KKE.喀喇昆仑断裂；WKL.西昆仑北缘断裂；TFF.塔拉斯费尔干纳断裂

Fig. 1. Simplified geological map in NE Pamir

下载: 全尺寸图片幻灯片

图 2 奥依塔格地区地质简图(据新疆大学，新疆地矿局塔里木盆地西南坳陷喀什凹陷南部石油地质综合研究总结报告，2001)

Fig. 2. Simplified geological map in Oytag area

下载: 全尺寸图片幻灯片

图 3 奥依塔格剖面综合柱状图及统计点野外照片(古流据Sobel, 1995)

Site8.现今河滩(38°58′52.8″N、75°31′16.5″E)杂乱堆积，未成岩，以巨砾和中砾为主，多呈近圆状-长条状，多呈次棱角状磨圆，分选中等；Site7.Q₂wq(39°01′06.3″N、75°33′33.4″E)杂乱堆积，未成岩，以巨砾和中砾为主，多呈近圆状-长条状，次棱角-次圆状磨圆，分选差；Site6.N₂a¹(38°59′20.1″N、75°32′11.4″E)以巨砾为主，多呈近圆状，次为长条状，次棱角-次圆状磨圆，分选中等，颗粒支撑，砂质填隙；Site5.N₂a¹(38°59′20.5″N、75°32′03.4″E)以巨砾为主，多呈近圆状，次为长条状，次圆-次棱角状磨圆，分选差，颗粒支撑，砂质填隙；Site4.N₂a¹(38°59′17.8″N、75°31′53.7″E)以巨砾为主，多呈次圆状，次为长条状，次棱角-次圆状磨圆，分选中等，颗粒支撑，砂质填隙；Site3.N₁p(38°59′05.2″N、75°30′50.7″E)以巨砾为主，多呈近圆状，次圆状磨圆，分选差，颗粒支撑，砂泥质填隙；Site2.N₁a(38°59′13.2″N、75°30′02.3″E)以巨砾为主，多呈近圆状，次为长条状，次棱角-棱角状磨圆，分选中等，颗粒支撑，砂泥质填隙；Site1.(E₃-N₁)_k(38°59′13.3″N、75°29′30.9″E)以巨砾为主，多呈近圆状，次棱角-棱角状磨圆，分选中等，颗粒支撑，砂泥质填隙

Fig. 3. Stratigraphical column and photos of 8 sites in Oytag section

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图 4 砾石统计结果

a.砾石成分统计结果；b.砾石磨圆统计结果；c.砾石粒径统计结果；d.砾石圆度统计结果

Fig. 4. Column of gravel counting data in Oytag section

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图 5 奥依塔格剖面Φ值转换后粒度分布方格图及累积概率分布及拟合曲线

Fig. 5. Histogram, cumulative frequency polygon and related fitting curve of Φ transformed grain size data in Oytag section

下载: 全尺寸图片幻灯片

表 1 奥依塔格剖面不同层位砾石统计结果

Table 1. Gravel counting results of 8 sites in Oytag section

统计点	Site1		Site2		Site3		Site4		Site5		Site6		Site7		Site8
统计点	F	F(%)	F	F(%)	F	F(%)	F	F(%)	F	F(%)	F	F(%)	F	F(%)	F	F(%)
岩性
火成岩	213	51.1	121	75.2	133	44.3	148	48.7	167	67.6	134	49.1	72	26.7	53	20.7
燧石	10	2.4	2	1.2	136	45.3	59	19.4	46	18.3	80	29.3	18	6.7	52	20.3
变质岩	102	24.4	21	13.0	27	9.0	97	31.9	36	14.3	33	12.1	84	31.1	133	51.9
砂岩	92	22.1	17	10.6	2	0.7	0	0.0	2	0.8	26	9.5	96	35.5	12	4.7
白云岩	0	0.0	0	0.0	2	0.7	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0
灰岩	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0	3	1.2
石膏	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0	1	0.4
泥岩	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0	1	0.4
小计	417	100	161	100	300	100	304	100	251	100	273	100	270	100	256	100
磨圆度
磨圆状	0	0.0	0	0.0	0	0.0	0	0.0	1	0.4	0	0.0	0	0.0	0	0.0
次磨圆状	18	4.3	26	16.1	222	74.0	176	57.9	122	48.6	93	34.0	98	36.3	38	14.8
次棱角状	304	72.9	93	57.8	59	19.7	115	37.8	112	44.6	173	63.4	156	57.8	193	75.4
棱角状	95	22.8	42	26.1	19	6.3	13	4.3	16	6.4	7	2.6	16	5.9	25	9.8
小计	417	100	161	100	300	100	304	100	251	100	273	100	270	100	256	100
圆度X(砾石长短轴直径比)
1≤X＜2	334	80.1	136	84.5	277	92.3	250	82.2	231	92.0	219	80.2	258	95.6	231	90.2
2≤X＜3	59	14.1	25	15.5	23	7.7	48	15.8	18	7.2	50	18.3	10	3.7	23	9.0
3≤X	24	5.8	0	0.0	0	0.0	6	2.0	2	0.8	4	1.5	2	0.7	2	7.8
小计	417	100	161	100	300	100	304	100	251	100	273	100	270	100	256	100
粒径(块)
小砾	415	99.5	158	98.1	291	97.0	294	96.7	246	98.0	271	99.3	150	55.6	134	52.3
中砾	2	0.5	3	1.9	9	3.0	10	3.3	5	2.0	2	0.7	120	44.4	120	46.9
巨砾	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0	0	0.0	2	0.8
小计	417	100	161	100	300	100	304	100	251	100	273	100	270	100	256	100

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表 2 奥依塔格剖面砾石长轴长度Φ值分布统计量

Table 2. Distribution of length counting data (Φ) in Oytag section

	Site1	Site2	Site3	Site4	Site5	Site6	Site7	Site8
均值	-4.18	-4.52	-4.15	-4.32	-4.26	-4.18	-5.82	-6.00
标准方差	0.90	0.93	1.00	1.15	1.03	0.90	1.11	0.97
偏斜度	-0.24	0.56	0.81	0.79	0.19	-0.24	-0.37	0.24
峰度	1.11	0.78	0.60	1.06	0.60	0.52	0.70	0.75

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