Development stage of Jurassic Che-Mo Paleouplift in the Junggar Basin and its constraints on sedimentary system
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摘要:研究目的
准噶尔盆地车—莫同沉积古隆起是影响侏罗系结构样式和储层分布特征的重要地貌单元，研究其发育过程有利于认识准噶尔盆地盆山耦合关系和油气藏的聚集规律。
研究方法本文基于盆地腹部41口井的测井数据和地震资料，对侏罗系砂体和地层结构进行了详细分析和等时性对比，重点阐述车—莫古隆起阶段性发育与准噶尔盆地周缘造山带，尤其是博格达山的协同演化及这种协同演化对盆地边界和沉积格局等的影响。
研究结果车—莫古隆起在侏罗纪的演化可划分为初始发育、快速隆升和隆升后剥蚀等三个阶段。早侏罗世车—莫古隆起的初始发育对八道湾组和三工河组展布和结构样式没有影响或影响很小，研究区由西北部扎伊尔山和东北部克拉美丽山供源，主要形成辫状河三角洲沉积体系；中侏罗世为车—莫古隆起的快速隆升阶段，除了西北部扎伊尔山和东北部克拉美丽山供源之外，博格达山也同步隆出水面开始供源，导致盆地边界、地层分布及结构样式的重大转变，使得西山窑组一段、二段大面积超覆、西山窑组三段沉积缺失或遭受剥蚀，沉积体系也随之发生转变，形成辫状河三角洲和滩坝共存的沉积体系组合；中侏罗世晚期和晚侏罗世车—莫古隆起隆升出水面则导致头屯河组和齐古组的剥蚀缺失，形成了与白垩系的区域不整合面。
结论车—莫古隆起在侏罗纪的形成和演化不仅影响到盆地的沉积地貌，也使盆地边界、物源格局发生重大改变，并导致沉积体系、地层结构样式和分布规律等的显著变化。
创新点:探讨了车—莫古隆起阶段性发育与准噶尔盆地周缘造山带，尤其是博格达山的协同演化及这种协同演化对盆地边界和沉积格局等的影响。
Abstract:This paper is the result of oil and gas exploration engineering.
ObjectiveChe−Mo synsedimentary paleouplift in Junggar basin is an important geomorphic unit that affects the structural style and reservoir distribution characteristics of Jurassic. The study of its development process is helpful to understand the basin mountain coupling relationship and the accumulation law of oil and gas reservoirs in Junggar basin.
MethodsBased on the logging data and seismic data of 41 wells in the abdomen of the basin, this paper makes a detailed analysis and isochronous comparison of Jurassic sand body and stratigraphic structure, and focuses on the synergistic evolution between the phased development of Che−Mo paleouplift and the orogenic belt around Junggar basin, especially Bogda mountain, and its influence on the basin boundary and sedimentary pattern.
ResultsThe evolution of Che−Mo paleouplift can be divided into three stages: initial development stage, rapid uplift stage and post uplift denudation stage. The initial development stage of Early Jurassic Che−Mo paleouplift has no or little influence on the distribution and structural style of Badaowan Formation and Sangonghe Formation. The study area is supplied by Zhayier mountain in the northwest and Kelameili mountain in the northeast, mainly forming braided river delta sedimentary system; The Middle Jurassic was the rapid uplift stage of Che−Mo paleouplift. In addition to the source supply of Zhayier mountain in the northwest and Kelameili mountain in the northeast, Bogda mountain also rose out of the water at the same time and began to supply the source, resulting in significant changes in basin boundary, stratigraphic distribution and structural style, resulting in large−area overlap of the first and second members of Xishanyao Formation, loss or denudation of the third members of Xishanyao Formation, The sedimentary system combination of Braided River Delta and beach bar is formed; The uplift of Che−Mo paleouplift in late Middle Jurassic and late Jurassic resulted in the denudation loss of Toutunhe Formation and Qigu Formation, forming a regional unconformity with Cretaceous.
ConclusionsThe formation and evolution of Che−Mo paleouplift in Jurassic not only affected the sedimentary landform of the basin, but also significantly changed the basin boundary and provenance pattern, and led to significant changes in sedimentary system, stratigraphic structure style and distribution law.
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Keywords:
- Che−Mo paleouplift /
- Jurassic /
- sedimentary system /
- tectonic evolution /
- Junggar Basin
Highlights:The co-evolution of the staged development of the Che−Mo paleouplift and the orogenic belt around the Junggar Basin, especially the Bogda Mountains, and the impact of this co-evolution on the basin boundary and sedimentary pattern are discussed.
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图 1 准噶尔盆地的位置及区域地质背景（a据徐学义等，2016修改）
1—中新生代盆地；2—前南华系基底上板内裂谷；3—古生代褶皱基底上板内裂谷；4—红海式裂谷；5—火山弧+岩浆弧；6—火山岛弧；7—早中泥盆世洋壳残片带；8—早古生代弧盆系及蛇绿混杂岩带；9—外陆棚沉积盆地；10—火山岛弧；11—岩浆弧；12—缝合带（蛇绿混杂岩带）；13—弧前增生楔；14—上叠盆地；15—陆缘裂谷；16—高压及超高压变质岩；17—超镁铁质岩；18—辉长岩及辉长-辉绿岩；19—地球物理探测的断裂带；20—韧性断裂带；21—走滑断裂；22—缝合带边界断裂及一级构造单元边界断裂；23—二级构造单元边界断裂；24—三级构造单元边界断裂及区域性大型断裂；25—井位及井号
Figure 1. The location and regional geological background of the Junggar Basin(Fig.a modified from Xu Xueyi et al., 2016)
1−Meso−Cenozoicbasin; 2−Intraplate rift on the Prenanhua basement system; 3−Intraplate rift onPaleozoic foldedbasement; 4−Red Sea type rift; 5−Volcanic arc+Magmatic arc; 6−Volcanic island−arc; 7−Early−Middle Devonian oceanic crustal debris belt; 8−Early Paleozoic arc basin system and ophiolitic mélange belt; 9−Outer shelf sedimentary basin; 10−Volcanic island−arc; 11−Magmatic arc; 12−Suture zone (ophiolite mélange belt); 13−Forearc accretive wedge; 14−Superimposed basin; 15−Marginal rift; 16−High pressure and ultrahigh pressure metamorphic rocks; 17−Ultramafic rocks; 18−Gabbro and gabbro−diabase; 19−Geophysically detected fault zone; 20−Ductile fault zone; 21−Strike−slip fault; 22−Boundary fault of primary tectonic unit; 23−Boundary fault of secondary tectonic unit; 24−Boundary fault of tertiary tectonic unit; 25−Well location and well number
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图 2 准噶尔盆侏罗系（沙1井）综合柱状图及等时性地层划分
Figure 2. Jurassic composite histogram of Well−Sha1 and isochronous stratigraphic division of Junggar Basin
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图 3 八道湾组区域砂体组合对比（剖面位置见图1）
Figure 3. Comparison of sand body combination in Badaowan Formation area (see Fig. 1 for section position)
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图 5 西山窑组区域砂体组合对比（剖面位置见图1）
Figure 5. Comparison of sand body combination in Xishanyao Formation area (see Fig. 1 for section position)
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图 6 车—莫古隆起区周缘地区西山窑组各段地层厚度反映的地层缺失和超覆特征
a—西山窑组一段等厚图；b—西山窑组二段等厚图；c—西山窑组三段等厚图
Figure 6. Stratum loss and overlap characteristics reflected by the stratum thickness of each section of Xishanyao Formation in the peripheral area of Chepaizi−Mosuowan paleouplift area
a–Isopach map of the first member of Xishanyao Formation; b–Isopach map of the second member of of Xishanyao Formation; c–Isopach map of the third member of ofXishanyao Formation
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图 7 研究区物源格局平面展布
a—三工河组二段沉积体系；b—西山窑组一段沉积体系；c—西山窑组二段沉积体系
Figure 7. Plane distribution of provenance pattern in the study area
a–Sedimentary system of the second member of Sangonghe Formation; b–Sedimentary system of the first member of Xishanyao Formation; c–Sedimentary system of the second member of Xishanyao Formation
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