南襄盆地泌阳凹陷深水湖底扇厘定及碎屑锆石U-Pb年代学物源追踪

张建光; 姚光庆; 陈亚兵; 樊中海; 林社卿; 杨永利

doi:10.3799/dqkx.2011.116

南襄盆地泌阳凹陷深水湖底扇厘定及碎屑锆石U-Pb年代学物源追踪

doi: 10.3799/dqkx.2011.116

张建光^{1, 2,},
姚光庆^{1, 2},
陈亚兵^{1, 2},
樊中海³,
林社卿³,
杨永利³

1.
中国地质大学资源学院, 湖北武汉 430074
2.
中国地质大学构造与油气资源教育部重点实验室, 湖北武汉 430074
3.
中国石油化工股份有限公司河南油田分公司石油勘探开发研究院, 河南南阳 473132

基金项目:

中国石油化工股份有限公司河南油田分公司石油勘探开发研究院课题 G0503-09-ZS-093

详细信息

作者简介:
张建光(1983-), 男, 博士研究生, 主要从事沉积学及储层地质学方面研究.E-mail: eduzjg@163.com

中图分类号: P618
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出版历程
- 收稿日期: 2011-01-29
- 网络出版日期: 2021-11-10
- 刊出日期: 2011-06-15

Sub-Lacustrine Fan of Chengdian and Zircon U-Pb Ages and Constraint on Its Provenance in Biyang Depression, Nanxiang Basin, China

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Research Institute of Exploration and Development of Henan Oilfield, Branch Company of SINOPEC, Nanyang 473132, China

摘要

摘要: 针对南襄盆地泌阳凹陷程店深水区湖底扇沉积体, 进行了岩心、粒度、薄片、重矿等测试资料、砂体结构及地球物理响应的综合分析.结果发现, 湖底扇砂体横向与平面结构呈现孤立特征, 岩性总体偏细, 具粗粒岩性, 以块状岩相为主体, 显示出砂质碎屑流流态特点, 含波状层理和交错层理的层理发育的岩相, 2类岩相具分异粒度特征.湖底扇沉积体显示出明显重力流性质, 兼具牵引流特点, 为复合式搬运机制, 其发育受控阵发性洪水作用、盆地幕式旋转掀斜作用及沉积缓倾斜坡因素, 是深水背景下洪水成因湖底扇沉积.为追踪其物源, 分别从侯庄三角洲与湖底扇区选取砂岩样品, 进行碎屑锆石U-Pb定年分析, 结果显示: 程店湖底扇与侯庄三角洲区砂岩样碎屑锆石测点年龄分布具相似特征, 碎屑锆石表面年龄分布显示单峰特征, 集中在166~115Ma, 该年龄段锆石类型以岩浆成因为绝对主体, 含少量变质锆石; 同时在247~210Ma、475~412Ma、813~663Ma、3489~1692Ma几个主要年龄区间亦具一定数量碎屑锆石分布.综合多方面资料, 结合区域地质背景, 初步得出如下结论: 程店湖底扇砂体与北部侯庄三角洲砂体为同物源沉积组合, 源岩主体形成时代为中侏罗世-早白垩, 对应燕山构造阶段, 主体物源岩系为宽坪-陶湾群构造岩相带中南侧发育的燕山期岩浆岩系, 同时, 前晋宁期、晋宁期、加里东期及印支期热事件形成的变质岩系或岩浆岩亦可能具不同程度的贡献.
- 湖底扇 /
- 锆石U-Pb年龄 /
- 物源 /
- 南襄盆地 /
- 泌阳凹陷 /
- 沉积作用
Abstract: Aiming at Chengdian deep water sandstone in Biyang depression of Nanxiang basin, we analyzed the core, the particle size, thin section, heavy minerals testing materials, structure of sandbody and the geophysical response of sedimentary sandbody, and found that the sub-lacustrine fan is an isolated body with fine and coarse lithology which consists of mainly massive lithologic facies with the characteristics of sandy debris flow sediments, but wavy bedding and cross bedding lithologic facies, two lithologic facies have its own particle-size feature, which shows the feature of turbidity current and tractive current.It's controlled by the paroxysmal flood, the revolving tilted effect and a gentle slope, we define it as a flood cause sub-lacustrine fan of composite transportation. In order to trace its provenance using clastic zircons dating analysis of sandstone samples, we selected samples from Chengdian sub-lacustrine and the Houzhuang delta area. The result shows: zircons microarea apparent ages of Chengdian sub-lacustrine and Houzhuang delta mainly similarly distribute between 115Ma and 166Ma with single peak and the magmatic zircons occupy the main part, with a few metamorphic zircons. Also, there are some different type zircons distributing in the age populations of 247-210Ma, 475-412Ma, 813-663Ma and 3489-1692Ma. In combination with regional geological settings and detritus zircon ages and heavy minerals composition, the authors come to the following preliminary conclusions: the sub-lacustrine sandbody derived from Houzhuang delta and its source rocks formation period is early Cretaceous to middle Jurassic, corresponding to Yanshan tectonic stage. Moreover, the source area is mainly Yanshanian granite in Kuanping-taowan tecnoic rock facies belt, including Yanshanian metamorphic rocks and the metamorphic rocks or magmatic rocks of Prejinningian period, Jinningian period, Caledonian period and Indosinian period may offer contributions to different degree.
- sub-lacustrine fan /
- zircon U-Pb ages /
- provenance /
- Nanxiang basin /
- Biyang depression /
- sedimentation

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图 1 南襄盆地大地构造位置、基底结构及泌阳凹陷核三上亚段沉积背景

①卢氏-确山断裂；②栾川-方城-明港断裂；③朱阳关-夏馆-大河断裂；④商南-镇平-松扒断裂；⑤丹凤-内乡-桐柏断裂；⑥下二门断裂；⑦曲洼断裂

Fig. 1. The location and basement structure of Nanxiang basin and the sedimentary settings of H₃U member of Biyang depression

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图 2 泌阳凹陷湖底扇沉积体典型沉积构造岩心

a.深灰色水平纹理钙片页岩，C2井，2811.08m；b.黑色页岩，深水背景沉积产物，岩心中也可见白云质泥岩等深湖环境产物，C2井，2780.22m；c.灰色平行层理中粗砂岩，C2井，2794.6m；d.深棕色含油细砂岩，洼状交错层理，暗示了牵引流流态，C1井，2760.85m；e.灰色粉细砂岩，上部波状层理，伴生生物遗迹构造，下部液化脉构造，暗示了古沉积期液化作用的存在，岩心序列中偶见，B365井，2716.22m；f.褐色含油细砂岩，小型槽状交错层理，底部与泥岩冲刷接触，冲刷与交错层理的结合反映了牵引流的存在，C1井，2764.5m；g.砂质泥岩表面线模构造，水流较强时形成，C1井，2766.2m；h.黑色泥岩夹薄层砂，C2井，2749.12m；i.下部灰色粉砂岩，上部各种各样泥碎屑以各种不同的形状分布于砂岩中，显示泥成塑性态于砂岩，C2井，2789.54m；j.上部泥砾呈漂浮状，C1井，2758.8m；k.褐色含油细砂岩夹3~4cm黑色泥岩，C1井，2764.05m；l.灰白色粗砂岩，含泥砾屑，略显定向排列，B365井，2710.90m；m.碳化植物碎屑，赋存于粉-细砂岩，密集成层分布，侧面上显现为层理，系碎屑流悬浮负载沉积产物，B365井，2713.50m；n.褐色含油中砂岩过渡到砂砾岩，中部石英颗粒呈漂浮状，C1井，2768.20m；o.块状砂砾岩，系碎屑流沉积产物，B365井，2713.2m；p.褐色含油块状层理细砂岩，C1井，2764.80m；q.灰色细砂岩，包卷变形层理，记录了沉积时期的液化作用和液化层的侧向流动的沉积过程，岩心序列中偶见，C1井，2760.52m；r.顶部灰白色疏松含砾粗砂岩，中部冲刷面，底部液化变形构造，B365井，2717.90m

Fig. 2. Typical sedimentary structures of the sub-lacustrine fan deposition in Biyang depression

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图 4 湖底扇砂岩岩屑成分及重矿物组成

Fig. 4. Detritus and heavy minerals composition of the sub-lacustrine fan sandstone

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图 3 湖底扇砂岩粒度概率累积曲线与C-M图(N、P、Q、R为粒度段)

Fig. 3. Probability cumulative frequency curve and C-M diagram of the sub-lacustrine fan sandstone

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图 5 湖底扇沉积体地震相特征及湖盆中心区地层切片

Fig. 5. Seismic facies of sub-lacustrine fan and stratal slicing from the center of lake basin

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图 6 沿物源方位湖底扇沉积体联井剖面

Fig. 6. Wells profile of the sub-lacustrine fan deposition along the direction of provenance

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图 7 泌阳凹陷深水背景湖底扇成因模式

Fig. 7. Genetic model of the sub-lacustrine fan in deep water of Biyang depression

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图 8 南襄盆地泌阳凹陷砂岩碎屑锆石的²⁰⁷Pb/²³⁵U-²⁰⁶Pb/²³⁸U谐和图

Fig. 8. ²⁰⁷Pb/²³⁵U-²⁰⁶Pb/²³⁸U Concordia plots of sandstone detrital zircons of Biyang depression in Nanxiang basin

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图 9 南襄盆地泌阳凹陷砂岩样品中碎屑锆石年龄分布

Fig. 9. Detrital zircons age distribution of standstones from Biyang depression in Nanxiang basin

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表 1 湖底扇发育地层层理发育砂岩样品粒度参数

Table 1. Sandstone grain parameters of sub-lacustrine fan deposition

井号	深度(m)	ϕ平均值	标准偏差	偏度	尖度	萨胡值
B365	2718.60	0.6	1	0.77	2.99	16.37
B365	2719.75	-0.16	0.98	0.56	2.12	11.09
B365	2720.90	0.05	0.89	0.17	1.94	10.09
C1	2765.97	2.18	0.59	0.06	2.83	16.45
C1	2767.62	0.72	0.94	0.63	2.92	16.04
C1	2767.97	1.72	1.97	0.61	4.18	22.21
C1	2762.42	1.99	0.56	0.32	2.53	14.92
C1	2763.00	2.81	0.43	-0.19	3.48	20.24
C1	2764.37	1.49	1.44	2.8	13.98	76.12
C1	2764.72	1.34	1.57	0.41	4.81	25.71
C1	2768.77	2.08	2.95	1.39	3.28	16.29

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表 2 南襄盆地泌阳凹陷取样数据

Table 2. Samples data from Biyang depression of Nanxiang basi

取样区	样品编号	井号	深度(m)	层位	岩性	打点数
湖底扇	BY-1	C1	2763.12	H3Ⅳ1	细砂岩	45
	BY-2	C1	2768.77	H3Ⅳ1	细砂岩	15
	BY-3	B365	2708.0	H3Ⅲ5	细砂岩	48
	BY-4	B365	2716.0	H3Ⅲ5	粗砂岩	20
侯庄三角洲	BY-5	B155	2480.19	H3Ⅳ1	粉砂岩	45
侯庄三角洲	BY-6	B296	2412.76	H3Ⅲ5	细砂岩	45

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