Sediment Provenance and Its Direction of Yueguifeng Formation in Lishui-Jiaojiang Depression: Evidence from Detrital Zircon U-Pb Chronology and Heavy Minerals
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摘要: 月桂峰组是丽水-椒江凹陷的主力烃源岩层，但其物源的研究薄弱，给油气勘探带来较大的困难.通过锆石U-Pb测年和重矿物分析等方法，对月桂峰组物源特征、差异及其地质意义进行系统分析对比.结果显示：物源以中酸性火成岩为主，含有少量变质岩，年龄以130~100 Ma为主，主要含有锆石、赤褐铁矿和磁铁矿等稳定重矿物；椒江凹陷与丽水东次凹物源主要来自雁荡凸起，丽水西次凹物源主要来自闽浙隆起带；少量火成岩和变质岩来自研究区附近的基底；锆石圆度偏好和ZTR值较高，说明物源经过中长距离搬运，这有利于中酸性岩浆岩中的石英和长石矿物富集，形成抗压实较好的石英质砂岩储层.
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关键词:
- 物源分析 /
- 锆石U-Pb同位素定年 /
- 重矿物分析 /
- 矿床学
Abstract: Yueguifeng Formation is the main source rock in Lishui-Jiaojiang depression, but it's poor research on provenance which brings great difficulties to oil and gas exploration. Based on zircon U-Pb dating and heavy mineral analysis, it was systematically analyzed and compared for the provenance characteristics, differences and geological significance of the Yueguifeng Formation. The results show that the provenance is mainly medium-acid igneous rocks main ages of which are 130-100 Ma with a small amount of metamorphic rocks, mainly containing stable heavy minerals such as zircon, hematite and magnetite. The provenance of Jiaojiang depression and east Lishui sub-depression mainly came from Yandang uplift, and the provenance of west Lishui sub-depression mainly came from Fujian-Zhejiang uplift. A small amount of igneous and metamorphic rocks came from the basement near the study area. Zircon roundness preference and ZTR values are higher, indicating that the provenance was transported over medium and long distances, which is conducive to the enrichment of quartz and feldspar minerals in medium-acid magmatic rocks, forming quartz sandstone reservoirs with good compaction resistance. -
图 1 丽水-椒江凹陷位置级构造单元及地层划分
Fig. 1. Division of position-level tectonic units and layer in Lishui-Jiaojiang depression
图 2 丽水-椒江凹陷砂岩碎屑锆石CL图像
Fig. 2. Clastic zircon CL images of sandstone in Lishui-Jiaojiang sag
图 3 丽水-椒江凹陷砂岩碎屑锆石Th/U比值
Fig. 3. Detrital zircon Th/U ratio of sandstone in Lishui-Jiaojiang sag
图 4 丽水-椒江凹陷砂岩碎屑锆石年龄谱和谐和图
Fig. 4. Detrital zircon age spectrum and concordant diagrams of sandstone in Lishui-Jiaojiang sag
图 5 月桂峰组物源综合分析图
红色箭头代表火山岩物源方向，黄色箭头代表变质岩物源方向，饼图代表重矿物组合百分比
Fig. 5. Comprehensive analysis of provenance of Yueguifeng Formation
表 1 丽水-椒江凹陷月桂峰组锆石Th和U元素及其比值
Table 1. Zircon Th and U elements and their ratios in the Yueguifeng Formation, Lishui-Jiaojiang sag
井号 深度(m) 锆石
颗数Th(10-6)* U(10-6)* Th/U* Th/U < 0.4
锆石颗数W1 3 526~3 554 80 20.38~2 198.48 (598.31) 154.52~2 666.54 (767.49) 0.01~2.05 (0.96) 5 W2 2 514~2 523 55 12~750 (225.62) 23.60~792 (289.90) 0.38~1.21 (0.78) 1 W3 3 708~3 720 59 58~762 (273.67) 64.30~1 157.00 (326.36) 0.06~1.84 (0.90) 5 N1 3 999~4 011 53 24~502 (170.77) 25.8~1 412.00 (277.21) 0.11~1.73 (0.80) 7 注：*最小值~最大值(均值). 
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表 2 丽水-椒江凹陷月桂峰组锆石年龄特征
Table 2. Zircon age characteristics of Yueguifeng Formation in Lishui-Jiaojiang sag
井号 深度(m) 岩浆锆石年龄(Ma) 变质锆石年龄(Ma) 主要年龄 年轻年龄 偏老年龄 W1 3 526~3 554 130~105 78~73 220~159 175~171、894、1 224、1 485 W2 2 514~2 523 126~103 82~75 245~183 - W3 3 708~3 720 122~100 89~75 245~183、328 204~222、328、1 562、1 850 N1 3 999~4 011 128~103 90 151~226、
409~475158、173~199、261~277、
1 369~1 515、1 860~2 013
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表 3 月桂峰组重矿物分类及平均百分比含量(%)
Table 3. Classification and average percentage content of heavy minerals in Yueguifeng Formation (%)
井号 超稳定 稳定 一般
稳定不稳定 锆石 电气石 金红石 合计 石榴石 磁铁矿 白钛矿 赤褐铁矿 锐钛矿 其他 合计 W2井 31.2 - 0.7 31.9 3.5 5.0 5.7 52.5 - - 66.7 0.7 0.7 A井 16.1 0.2 - 16.3 2.4 7.8 1.6 67.2 0.9 0.9 80.8 0.3 2.6 B井 8.1 0.3 0.7 9.0 0.3 1.1 1.1 88.3 0.3 - 91.0 - - L1井 35.6 0.1 0.2 36.0 1.1 0.2 59.7 0.2 2.0 0.6 63.8 - 0.2 W3井 30.8 0.7 0.4 31.9 7.2 2.3 47.9 6.0 3.2 - 66.5 1.1 0.4 N1井 47.7 1.9 1.2 50.8 2.3 30.6 12.0 3.4 0.8 - 49.1 - 0.1
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