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本溪地区本溪组沉积有机质演化

发布时间:2018-01-30 04:13

  本文关键词: 本溪组 镜质体反射率 埋藏史 有机质演化 出处:《沈阳师范大学》2015年硕士论文 论文类型:学位论文


【摘要】:石炭纪地层在我国华北地区分布广泛,在辽东地区,石炭纪地层十分发育。其中,本溪组是一套海陆交互相的地层,也是这一地区具有代表性的地层。本溪组地层在本溪地区出露地点分别是位于本溪市西北的牛毛岭、偏岭乡窑子峪、田师付镇孔家堡子地区,其中,牛毛岭剖面是本溪组的命名剖面。近百年来,很多地质古生物学家对本溪组的古生物和地层都进行了较为详细的探究。在此基础上,本论文着重研究本溪地区本溪组的沉降史及沉积有机质演化。本文研究了牛毛岭本溪组标准剖面、窑子峪本溪组剖面和田师付孔家堡子本溪组剖面的岩性及沉积层序,对窑子峪本溪组剖面进行了实际测量并进行了岩性分析。在三条剖面共采集Ro标本9个,并选择其中的4个样品进行了镜质体反射率的检测,其结果表明这一地区本溪组的有机质演化程度可达长焰煤—贫煤阶段。通过绘制相关的沉降史曲线图,分析本溪组煤系地层的埋藏史,认为这一地区的沉降史大致分为前期、中期和后期三个阶段,分别为缓慢沉降期、快速沉降期和抬升期。这一地区本溪组的古地理环境总体表现为河流到滨岸沼泽再到海陆交互相沉积的过程。
[Abstract]:Carboniferous strata are widely distributed in North China, and Carboniferous strata are well developed in the eastern part of Liaoning Province. Benxi formation in Benxi area is located in Niumoling, Yaoziyu, Yaoziyu, Tianshifu town, which is located in the northwest of Benxi city. Niumaoling section is a named section of Benxi formation. In the last hundred years, many geobiologists have studied the paleontology and strata of Benxi formation in detail. In this paper, the sedimentation history and the evolution of sedimentary organic matter of Benxi formation in Benxi area are studied, and the standard section of Niumaoling Benxi formation is studied in this paper. The lithology and sedimentary sequence of the section of the Yanziyu Benxi formation and the section of Fukongjiapuzi Benxi formation are measured and analyzed. Nine samples of Ro are collected in three sections. Four of the samples were selected for vitrinite reflectance detection. The results show that the evolution degree of organic matter in Benxi formation in this area can reach the stage of long flame coal and lean coal. By analyzing the burial history of coal measure strata in Benxi formation, it is considered that the subsidence history in this area can be divided into three stages, namely, the early stage, the middle stage and the later stage, respectively, which are the slow subsidence periods. The paleogeographic environment of Benxi formation in this area is the process of river to shore swamp and then to sea and land intersecting each other.
【学位授予单位】:沈阳师范大学
【学位级别】:硕士
【学位授予年份】:2015
【分类号】:P618.11

【参考文献】

相关期刊论文 前9条

1 米家榕,孙克勤,金建华;辽宁本溪早石炭世植物化石[J];长春地质学院学报;1990年04期

2 金建华;辽东太子河流域“本溪组”涵义的厘定[J];地层学杂志;1995年03期

3 蒋国豪,胡瑞忠,方维萱;镜质体反射率(R_O)推算古地温研究进展[J];地质地球化学;2001年01期

4 高金汉;王训练;王燕;王艳丽;;辽宁本溪牛毛岭石炭系本溪组腕足动物群落及其古环境意义[J];古地理学报;2007年05期

5 范国清;;辽宁石炭纪海侵[J];辽宁地质;1987年02期

6 王岚,R.P.Suggate;埋藏深度、镜质体反射率和地温梯度的关系[J];海洋石油;1998年04期

7 郎嘉彬;王成源;;本溪组命名剖面牙形刺动物群的特征及地质时代[J];世界地质;2007年02期

8 陆春生,,漆家福,陆克政;沉降模拟的模型改进及系统研制[J];应用基础与工程科学学报;1996年04期

9 金建华,米家榕;辽宁本溪田师傅早中石炭世沉积环境分析[J];中山大学学报(自然科学版);1999年05期

相关硕士学位论文 前1条

1 郎嘉彬;辽宁本溪石炭系本溪组命名剖面的牙形刺化石[D];吉林大学;2007年



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