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三塘湖盆地马朗凹陷卡拉岗组火山岩岩性及岩相特征研究

梁浩 苟红光 王志矿 崔娥 孟旺才 张志更

沉积学报2011,Vol.29Issue(6):1156-1163,8.
沉积学报2011,Vol.29Issue(6):1156-1163,8.

三塘湖盆地马朗凹陷卡拉岗组火山岩岩性及岩相特征研究

Characteristics of Lithology and Lithofacies of Kalagang Volcanic Rocks in Malang Depression,Santanghu Basin

梁浩 1苟红光 2王志矿 2崔娥 2孟旺才 2张志更2

作者信息

  • 1. 中国地质大学资源学院能源地质工程,武汉430074
  • 2. 中国石油吐哈油田分公司勘探开发研究院,新疆哈密839009
  • 折叠

摘要

Abstract

Comparison and classification of volcanic rocks are the premise and foundation of their lithology research,lithofacies and variation.According to log data,seismic data and pollen analysis,we found that the Kalagang volcanic rocks of Malang depression in Santanghu Basin were thick in the north and east,thin in the south and westareas.The pollen assemblage showed that Gymnosperm pollen had a clear advantage in fern spores and comprised of Genus Cordaitina(Samoilovichi) Hart,Genus Florinites Sehof,WilSonet Bentall,Genus Protohaploxypinus(Samoilovichi) Hart,Genus Striatoabieites(Sedova) Hartpollen.The content of Genus Cordaitina(Samoilovichi) Hart was up to 25.3~54.3%.Compared the log response of Kalagang volcanic rocks and Sedimentary rocks,there performed low natural gamma,low acoustic time,low compensation neutrons,high density and high resistance.The natural gamma value of Kalagang volcanic rocks was lower than Harjiawu Formation,while the resistance was higher.The lithology was mainly mafic-neutral basalt and andesite,and minor of the tuff,tuffite,volcanic breccia,and so on.Kalagang volcanic rocks of Malang depression can be divided into outbreak phase,overflow phase and volcanic sediment facies.The volcanic activity mainly occurred as a relatively quiet overflow phase,followed by strong eruption phase,and locally developed volcanic sediment facies.

关键词

马朗凹陷/卡拉岗组/火山岩岩相

Key words

Malang depression/Kalagang Formation/volcanic lithofacies

分类

能源科技

引用本文复制引用

梁浩,苟红光,王志矿,崔娥,孟旺才,张志更..三塘湖盆地马朗凹陷卡拉岗组火山岩岩性及岩相特征研究[J].沉积学报,2011,29(6):1156-1163,8.

基金项目

中国石油天然气股份有限公司科技研发项目(编号:2008B-01)资助 ()

沉积学报

OA北大核心CSCDCSTPCD

1000-0550

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