准噶尔盆地东部构造特征及演化定量分析

马超; 吴孔友; 裴仰文; 李天然

doi:10.12090/j.issn.1006-6616.2019.25.03.029

准噶尔盆地东部构造特征及演化定量分析

doi: 10.12090/j.issn.1006-6616.2019.25.03.029

中国石油大学(华东)地球科学与技术学院, 山东青岛 266580

基金项目:

国家科技重大专项 2017ZX05001003-004

中科院先导A类专项 XDA14010301

详细信息

作者简介:
马超(1993-), 男, 在读硕士, 从事构造地质学研究方向。E-mail:2824659957@qq.com

中图分类号: P542
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- 被引次数: 0
出版历程
- 收稿日期: 2019-01-06
- 修回日期: 2019-03-06
- 刊出日期: 2019-06-01

QUANTITATIVE ANALYSIS OF TECTONIC CHARACTERISTICS AND EVOLUTION IN THE EASTERN JUNGGAR BASIN

School of Geosciences, China University of Petroleum, Qingdao 266580, Shandong China

摘要

摘要: 准噶尔盆地东部地区经历了多期次的构造运动，其构造特征和形成演化机制对该地区的油气勘探和开发具有十分重要的指导意义。运用高分辨率的二维、三维地震、测井数据，优选十条地质格架剖面开展精细构造解释，刻画出不同构造单元的地质结构特征，建立了跨各个构造单元的地质解译模型。在精细构造解译的基础上，基于平衡剖面恢复原理，通过Midland Valley的3D MOVE功能模块对10条地质格架剖面进行构造恢复，并对其各地质时期构造缩短量和缩短速率进行定量表征。准噶尔东部地区缩短量及缩短速率统计分析表明，在东西方向上，三叠纪至侏罗纪缩短量（4.60~11.28 km）及缩短速率最大（0.12~0.20 mm/a），这一时期准东地区经历了强烈的东西向挤压构造变形；在南北方向上，二叠纪和新近纪末期缩短量（2.56~8.93 km、0.54~6.90 km）及缩短速率最大（0.05~0.15 mm/a、0.02~0.19 mm/a），这两个时期准东地区经历了强烈的南北向挤压构造变形。
- 平衡剖面恢复 /
- 缩短量 /
- 缩短速率 /
- 构造演化 /
- 构造叠加
Abstract: The eastern Junggar Basin has undergone multiple tectonic movements. Its tectonic characteristics, formation and evolution mechanism are of great guiding value for oil and gas exploration and development in this area. By using high-resolution 2-D and 3-D seismic and well logging data, ten geological framework sections were selected to carry out fine tectonic interpretation, and the geological characteristics of different tectonic units were described, and the geological interpretation model across each tectonic unit was established. On the basis of fine tectonic interpretation and under the guidance of balanced profile restoration, the sections of ten geological frameworks were reconstructed through the 3D MOVE function module of Midland Valley, and the amount and rate of tectonic shortening in each geological period were quantitatively characterized. The results show that in the East-West direction, the shortening amount (4.60~11.28 km) and the shortening rate (0.12~0.20 mm/a) from the Triassic to the Jurassic periods were the largest and the Junggar region experienced intense East-West compressional tectonic deformation during this period. In the North-South direction, the shortening amount (2.56~8.93 km, 0.54~6.90 km) and the shortening rate (0.05~0.15 mm/a, 0.02~0.19 mm/a) at Permian and the end of Neogene periods were the largest and the Jundong region underwent intense North-South compressional tectonic deformation.
- balanced profile restoration /
- shortening amount /
- shortening rate /
- tectonic evolution /
- structural superposition
注释:

责任编辑:范二平

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图 1 研究区构造背景及剖面位置

a—准噶尔盆地及周缘界山；b—准噶尔盆地构造单元划分（据新疆油田）；c—准噶尔盆地东部地区构造格局及地质格架剖面位置

Figure 1. Tectonic background and section location of the study area

下载: 全尺寸图片幻灯片

图 2 地质格架剖面D-D′地震解译(剖面位置见图 1c)

a—原始地震剖面；b—构造解译方案

Figure 2. Seismic interpretation of geological section D-D′ (Section position is shown in Figure 1c)

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图 3 地质格架剖面G-G′地震解释(剖面位置见图 1c)

a—原始地震剖面；b—构造解译方案

Figure 3. Seismic interpretation of geological section G-G′ (Section position is shown in Figure 1c)

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图 4 地质格架剖面D-D′构造演化图(剖面位置见图 1c)

Figure 4. Tectonic evolution of geological section D-D′ (Section position is shown in Figure 1c)

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图 5 地质格架剖面D-D′缩短量和缩短速率

Figure 5. Statistics of section D-D′ including shortening amount and shortening rate

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图 6 地质格架剖面G-G′构造演化图(剖面位置见图 1c)

Figure 6. Tectonic evolution of geological section G-G′ (Section position is shown in Figure 1c)

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图 7 地质格架剖面G-G′缩短量和缩短速率

Figure 7. Statistics of section G-G′ including shortening amount and shortening rate

下载: 全尺寸图片幻灯片

图 8 准东地区南北向地质格架剖面缩短量及缩短速率

Figure 8. Statistics of the E-W geological sections, demonstrating shortening amounts and shortening rate

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图 9 准东地区东西向地质格架剖面缩短量及缩短速率

Figure 9. Statistics of the N-S geological sections, demonstrating shortening amounts and shortening rate

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图 10 准东地区早二叠世以来三维构造演化模型

a—早二叠世；b—中二叠世；c—早三叠世；d—侏罗纪

Figure 10. The 3D structural evolution models of eastern Junggar Basin since Early Permian

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表 1 东西向剖面缩短量及缩短速率数据统计表

Table 1. Statistic dataset of shortening amounts (km) and shortening rates (mm/a) of E-W geological sections

	缩短量/km				缩短速率/(mm/a)
	A-A′	B-B′	C-C′	D-D′	A-A′	B-B′	C-C′	D-D′
P沉积前	—	—	—	—	—	—	—	—
T沉积前	2.20028	1.86994	2.45878	1.88073	0.04681	0.03979	0.05231	0.04002
J沉积前	4.60112	6.85644	8.60574	7.52291	0.12257	0.13444	0.16874	0.14751
K沉积前	4.25007	6.23312	6.55676	11.28437	0.12682	0.11131	0.11708	0.20151
E沉积前	0.55007	2.49325	0.40980	5.01527	0.00696	0.03156	0.00519	0.06348
N沉积前	—	0.62331	1.22939	1.25382		0.01450	0.02859	0.02916
现今	2.75035	0.62327	0.40980	1.25382	0.04167	0.02710	0.01782	0.05451

下载: 导出CSV

表 2 南北向剖面缩短量及缩短速率数据统计表

Table 2. Statistic dataset of shortening amounts (km) and shortening rates (mm/a) of N-S geological sections

	缩短量/km					缩短速率/(mm/a)
	F-F′	G-G′	H-H′	I-I′	J-J′	F-F′	G-G′	H-H′	I-I′	J-J′
P沉积前	—	—	—	—	—	—	—	—	—	—
T沉积前	6.58858	8.92584	2.56280	6.63796	6.75319	0.14018	0.14736	0.05453	0.14123	0.14368
J沉积前	1.49740	4.43114	1.64751	2.80837	2.43115	0.02936	0.12610	0.03230	0.05507	0.04767
K沉积前	1.49740	2.47352	1.09834	0.76592	1.89089	0.02674	0.04417	0.01961	0.01368	0.03377
E沉积前	1.19792	0.98941	0.91529	0.51061	0.54026	0.01516	0.01252	0.01159	0.00646	0.00684
N沉积前	3.09169	2.49470	—	0.25531	0.27013	0.08143	0.01150	—	0.00594	0.00628
现今	4.39533	6.90465	1.28140	1.78714	0.54026	0.11719	0.18716	0.01942	0.07770	0.02349

下载: 导出CSV

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