首页|河南华北型寒武系馒头组微生物岩沉积特征研究

河南华北型寒武系馒头组微生物岩沉积特征研究

扫码查看
基于微生物碳酸盐岩的巨大能源前景、古环境意义和钙化机理,研究了河南省华北型寒武系第二统和第三统的馒头组32层微生物岩的沉积特征,并结合伴生沉积构造和岩相变化,对比分析了馒头组一、二、三段微生物岩沉积的相关性特征及其演化规律,认为从馒头组一段到三段微生物岩沉积层数和丰度呈减少趋势,一段叠层石和纹理石明显占优,三段以均一石为主.陆源物质(泥质)供应是导致河南省华北型寒武系馒头组微生物岩形态及沉积特征发生变化的直接因素,海平面的变化即水动力条件是造成微生物岩形态特征发生变化的决定因素,后生动物的大量出现则促进了微生物岩的消亡.研究结果表明:河南华北型寒武系馒头组微生物岩丰富,其中叠层石12层,纹理石13层,核形石2层,均一石5层;微生物岩的沉积特征是内因(微生物)和外因(环境条件)共同作用的结果.
Sedimentary characteristics of microbialites of the North China type in mantou formation Cambrian, Henan
Based on the huge energy prospects, palaeo-environmental significance and calcification mechanism, the current study researched on the sedimentary characteristics of microbialites of 32 layers, and contrastively analyzed the related characteristics and evolution law of microbialites in the first, second and third member of mantou formation, in combining the associated sedimentary structure and lithofacies change. The results show that the layer and abundance of microbialites decrease from the first member to the third member, and stromatolites and texture stones are obviously superior in the first member but uniform stones are the principal components in the third member. The supply of terrigenous sediment (muddy) is the direct factor that leads to the morphology and sedimentary characteristics change of microbialites, while the change of sea level, namely water power, is the decisive factor that triggers the change of morphological characteristics of microbialites. Additionally, emergence of many met-azoan stimulates the extinction of microbialites. The study results in the following conclu-siongs: the microbialites of the north china type in mantou formation Cambrian are rich in Henan province, precisely 12 layers of stromatolites, 13 layers of texture stones, 2 layers of oncolites and 5 layers of uniform stones; The sedimentary characteristics of microbialites result from the internal factors (microbe) and external factors (environmental conditions).

microbialitesedimentary characteristicscontrolling factorsmantou formationHenan province

常玉光、黄华州、郑伟、孙凤余

展开 >

河南理工大学资源环境学院河南省生物遗迹与成矿过程重点实验室,河南焦作454000

中国矿业大学资源与地球科学学院,江苏徐州 221116

微生物岩 沉积特征 控制因素 馒头组 河南省

国家自然科学基金国家自然科学基金河南省基础与前沿项目高等学校博士学科点专项科研基金河南省生物遗迹与成矿过程重点实验室开放基金

412020715110414811230041321320114116110001OTMP1002

2013

中国矿业大学学报
中国矿业大学

中国矿业大学学报

CSTPCDCSCD北大核心EI
影响因子:1.83
ISSN:1000-1964
年,卷(期):2013.42(2)
  • 4
  • 9