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克百断裂带上盘石炭系火山喷发期次划分与火山岩分布规律

高炎 陈建 姚宗全 汤传意 谢宗瑞 杨远峰 张欣 刘谨铭 王威 牟家园

东北石油大学学报2026,Vol.50Issue(1):1-13,13.
东北石油大学学报2026,Vol.50Issue(1):1-13,13.DOI:10.3969/j.issn.2095-4107.2026.01.001

克百断裂带上盘石炭系火山喷发期次划分与火山岩分布规律

Division of volcanic eruption stages and distribution on the hanging wall of the Carboniferous volcanic rocks in Kebai Fault Zone

高炎 1陈建 2姚宗全 2汤传意 1谢宗瑞 1杨远峰 1张欣 1刘谨铭 1王威 2牟家园2

作者信息

  • 1. 中国石油新疆油田分公司百口泉采油厂,新疆 克拉玛依 834011
  • 2. 新疆大学地质与矿业工程学院,新疆 乌鲁木齐 830047||新疆中亚造山带大陆动力学与成矿预测自治区重点实验室,新疆乌鲁木齐 830000
  • 折叠

摘要

Abstract

The volcanic rocks in the upper plate of the Kebai Fault Zone in the Carboniferous system ex-hibit complex and variable lithology and lithofacies,with multiple stages of volcanic rock superimposi-tion,resulting in chaotic seismic reflection characteristics and unclear hydrocarbon distribution patterns.Based on integrated geochemical,lithological,well-log,and seismic data,the tectonic setting,geolog-ical age,and petrological characteristics of the study area were clarified,leading to the establishment of criteria for dividing volcanic eruption cycles and stages,as well as defining the distribution patterns of volcanic rocks.Results indicate that the Kebai Fault Zone developed in an island-arc tectonic setting,with an age of approximately(316.8±2.9)Ma,and exhibits a lithofacies sequence transitional from vol-canic lava to pyroclastic rocks.One eruption cycle was identified in the study area,bounded primarily by unconformities and weathering crusts.The Carboniferous system in the Kebai Fault Zone can be divided into five stages(C1-C5):the C1 stage is dominated by andesite,with a sedimentary interlayer of tuf-faceous sandy conglomerate at the top;the C2 stage consists of interbedded andesite and tuffaceous sandy conglomerate,topped by a tuffaceous sandy conglomerate marking the stage boundary;the C3 and C4 stages are characterized by tuffaceous sandy conglomerate and tuff as key lithological and lithofa-cies indicators;the C5 stage develops tuffaceous sandy conglomerate,forming a weathering crust in un-conformable contact with the Jurassic strata.The Chemical Index of Alteration(CIA)values for stages C1-C5 show alternating intensity of alteration,reflecting periodic changes in weathering conditions.Laterally,volcanic lava extends from north to south with progressively reduced distribution and dimin-ished eruption intensity.These results provide guidance for characterizing the vertical sequence and spa-tial distribution of different volcanic stages in the study area.

关键词

克百断裂带/石炭系/构造环境/火山喷发期次/火山岩/岩性分布规律

Key words

Kebai Fault Zone/Carboniferous system/tectonic environment/periodization of volcanic e-ruptions/volcanic rocks/regularity of lithological distribution

分类

天文与地球科学

引用本文复制引用

高炎,陈建,姚宗全,汤传意,谢宗瑞,杨远峰,张欣,刘谨铭,王威,牟家园..克百断裂带上盘石炭系火山喷发期次划分与火山岩分布规律[J].东北石油大学学报,2026,50(1):1-13,13.

基金项目

国家自然科学基金项目(42572181) (42572181)

新疆维吾尔自治区重大科技专项项目(2025A01010-1) (2025A01010-1)

东北石油大学学报

2095-4107

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