本文關(guān)鍵詞： 本溪組 鏡質(zhì)體反射率 埋藏史 有機(jī)質(zhì)演化　出處：《沈陽(yáng)師范大學(xué)》2015年碩士論文　論文類型：學(xué)位論文

【摘要】：石炭紀(jì)地層在我國(guó)華北地區(qū)分布廣泛,在遼東地區(qū),石炭紀(jì)地層十分發(fā)育。其中,本溪組是一套海陸交互相的地層,也是這一地區(qū)具有代表性的地層。本溪組地層在本溪地區(qū)出露地點(diǎn)分別是位于本溪市西北的牛毛嶺、偏嶺鄉(xiāng)窯子峪、田師付鎮(zhèn)孔家堡子地區(qū),其中,牛毛嶺剖面是本溪組的命名剖面。近百年來(lái),很多地質(zhì)古生物學(xué)家對(duì)本溪組的古生物和地層都進(jìn)行了較為詳細(xì)的探究。在此基礎(chǔ)上,本論文著重研究本溪地區(qū)本溪組的沉降史及沉積有機(jī)質(zhì)演化。本文研究了牛毛嶺本溪組標(biāo)準(zhǔn)剖面、窯子峪本溪組剖面和田師付孔家堡子本溪組剖面的巖性及沉積層序,對(duì)窯子峪本溪組剖面進(jìn)行了實(shí)際測(cè)量并進(jìn)行了巖性分析。在三條剖面共采集Ro標(biāo)本9個(gè),并選擇其中的4個(gè)樣品進(jìn)行了鏡質(zhì)體反射率的檢測(cè),其結(jié)果表明這一地區(qū)本溪組的有機(jī)質(zhì)演化程度可達(dá)長(zhǎng)焰煤—貧煤階段。通過(guò)繪制相關(guān)的沉降史曲線圖,分析本溪組煤系地層的埋藏史,認(rèn)為這一地區(qū)的沉降史大致分為前期、中期和后期三個(gè)階段,分別為緩慢沉降期、快速沉降期和抬升期。這一地區(qū)本溪組的古地理環(huán)境總體表現(xiàn)為河流到濱岸沼澤再到海陸交互相沉積的過(guò)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.
【學(xué)位授予單位】：沈陽(yáng)師范大學(xué)
【學(xué)位級(jí)別】：碩士
【學(xué)位授予年份】：2015
【分類號(hào)】：P618.11

【參考文獻(xiàn)】

相關(guān)期刊論文 前9條

1 米家榕,孫克勤,金建華;遼寧本溪早石炭世植物化石[J];長(zhǎng)春地質(zhì)學(xué)院學(xué)報(bào);1990年04期

2 金建華;遼東太子河流域“本溪組”涵義的厘定[J];地層學(xué)雜志;1995年03期

3 蔣國(guó)豪,胡瑞忠,方維萱;鏡質(zhì)體反射率(R_O)推算古地溫研究進(jìn)展[J];地質(zhì)地球化學(xué);2001年01期

4 高金漢;王訓(xùn)練;王燕;王艷麗;;遼寧本溪牛毛嶺石炭系本溪組腕足動(dòng)物群落及其古環(huán)境意義[J];古地理學(xué)報(bào);2007年05期

5 范國(guó)清;;遼寧石炭紀(jì)海侵[J];遼寧地質(zhì);1987年02期

6 王嵐,R．P．Suggate;埋藏深度、鏡質(zhì)體反射率和地溫梯度的關(guān)系[J];海洋石油;1998年04期

7 郎嘉彬;王成源;;本溪組命名剖面牙形刺動(dòng)物群的特征及地質(zhì)時(shí)代[J];世界地質(zhì);2007年02期

8 陸春生，，漆家福，陸克政;沉降模擬的模型改進(jìn)及系統(tǒng)研制[J];應(yīng)用基礎(chǔ)與工程科學(xué)學(xué)報(bào);1996年04期

9 金建華,米家榕;遼寧本溪田師傅早中石炭世沉積環(huán)境分析[J];中山大學(xué)學(xué)報(bào)(自然科學(xué)版);1999年05期

相關(guān)碩士學(xué)位論文 前1條

1 郎嘉彬;遼寧本溪石炭系本溪組命名剖面的牙形刺化石[D];吉林大學(xué);2007年

本文編號(hào)：1475259