五大連池老黑山西部熔巖流的張裂特征及其成因分析

【中文摘要】 地質(zhì)張裂系統(tǒng)廣泛見(jiàn)于熔巖流、地面沉降和張性構(gòu)造發(fā)育的地區(qū)。而基性熔巖流的張裂體系具有獨(dú)特性,是地下水(或礦泉水)和油氣的重要儲(chǔ)體和運(yùn)移通道。本文通過(guò)對(duì)老黑山西部熔巖流的張裂體系的野外實(shí)地觀察,結(jié)合高分辨率的遙感圖象,對(duì)張裂體系的信息進(jìn)行了提取和分析,試圖探尋老黑山玄武質(zhì)熔巖流張裂體系的分布規(guī)律及其成因。五大連池老黑山西側(cè)熔巖流的張裂隙非常發(fā)育,長(zhǎng)短、寬窄不一。根據(jù)高分辨率QuickBird全色波段遙感數(shù)據(jù)可對(duì)張裂寬度大于0.5米和長(zhǎng)度大于3米的張裂可以分辨的能力,本次工作對(duì)老黑山西部熔巖流的張裂進(jìn)行了系統(tǒng)提取。所獲得的數(shù)據(jù)在地理信息系統(tǒng)軟件中進(jìn)行了空間分析。對(duì)張裂的空間分布特征的分析和描述包括張裂的分布方向、區(qū)域單位面積內(nèi)張裂的長(zhǎng)度、區(qū)域單位面積內(nèi)張裂的條數(shù)(即張裂的分布密度)。在張裂整體優(yōu)勢(shì)方向確定后,在研究區(qū)內(nèi)選取了15個(gè)張裂集中分布區(qū),分別統(tǒng)計(jì)了區(qū)內(nèi)張裂分布的特點(diǎn):優(yōu)勢(shì)方向、單位面積區(qū)域內(nèi)張裂的長(zhǎng)度、單位面積區(qū)域內(nèi)張裂的條數(shù)(即張裂的分布密度)。這些區(qū)域有些是屬于同期的熔巖流、有些則不是同期的熔巖流。它們的方向分布反映了該區(qū)域熔巖流的張裂特點(diǎn)。對(duì)五大連池老黑山西部熔巖流邊緣的一股較大規(guī)模次級(jí)溢流體上的熔巖穹丘的分析,得到了21個(gè)熔巖穹丘的面積、周長(zhǎng)和長(zhǎng)寬比信息。通過(guò)以上工作,得出了下面幾點(diǎn)結(jié)論性的認(rèn)識(shí):1.老黑山西部熔巖流的張裂分布存在著不同的組合結(jié)構(gòu),這些組合結(jié)構(gòu)與產(chǎn)生張裂的不同類型和期次的熔巖流之間存在著緊密的相關(guān)性。2.根據(jù)遙感影像判讀及實(shí)地觀察,老黑山西部熔巖流的張裂有三組優(yōu)勢(shì)方向,它們反映了熔巖流的流動(dòng)方向。大規(guī)模熔巖流的總流動(dòng)方向是東西向和北西向,而北東向的熔巖流可能是這些大規(guī)模熔巖流的次級(jí)溢流,甚至是更小規(guī)模的次級(jí)溢流。3.隨著距離老黑山火山錐位置的不同和熔巖流的類型(如席狀熔巖流、小規(guī)模次級(jí)溢流體)不同,張裂呈現(xiàn)不同的特征。

【英文摘要】 The geological systems of tension fissures are widely found in the regions of lava flows, ground subsidence and development of extension structures. However, the fissure systems on the basaltic lava flows are very outstanding, which are the important storage media and migration pathway of groundwater (or mineral water), oil and gas. Through the field observations of the tension fissures on the western lava flows of Laoheishan volcano and the uses of high-resolution remote sensing data, we explored and analyzed the information of the systems of tension fissures and attempt to reveal the law of their spatial distribution and their causes.The tension fissures on the western lava flows of Laoheishan volcano are very rich and have different length and width. According to the ability of high-resolution panchromatic band of Quickbird remote sensing data to identify the tension fissures with the width > 0.5 meter and the length of >3 meter, we took out the data of tension fissures on the western lava flows of Laoheishan volcano. Then the data were analyzed on their spatial distributions by the software of geographic information system. The spatial distribution characteristics of the tension fissures were also analyze and described, such as the distribution of fissure direction, the fissure length within unit area and the fissure number within unit area. After the determination of the overall advantage direction, we chose fifteen interest areas with amounts of tension fissures and studied the distribution characteristics of fissures in each interest areas, including advantage direction, the length and number of fissures within unit area.Some of these areas are the lava flows forming in the same period, while others are not. Their direction distributions reflect the characteristics of fissures in the area. In addition, we measured the information of area, perimeter and aspect ratio of twenty-one tumuli and lava collapse of larger sub-overflow in the edge of western lava flows of Laoheishan volcano, Wudalianchi. The conclusions are as follows:1. There exists the characteristic combination structures of the tension fissures in the western lava flows of Laoheishan volcano. These combination structures have close relationship with the different types and stages of lava flows.2. According to the interpretation of remote sensing data and the field observations, three groups of the fissure advantage-directions in the western lava flows of Laoheishan volcano are recognized, which reflects the directions of lava flows. The overall flow directions of large lava flows is east-west and north-west,but the north-east flow direction of lava flows may be the sub-overflow of large lava flows or the smaller ones.3. With the different distances between fissures and Laoheishan volcanic cone and the types of lava flows (sheet lava flows or small sub-overflows), the tension fissures show the different features.

【中文關(guān)鍵詞】 五大連池; 老黑山; 熔巖流; 熔巖穹丘; 張裂
【英文關(guān)鍵詞】 Wudalianchi; Laoheishan volcano; lava flow; tumulus; fissure
【畢業(yè)論文目錄】
摘要 4-5
ABSTRACT 5-6
第1章 引言 8-15
    1.1 基性熔巖流的張裂構(gòu)造研究進(jìn)展 8-12
        1.1.1 基性熔巖流 8-10
        1.1.2 基性熔巖流的張裂 10-12
    1.2 本文研究的主要對(duì)象和研究方法 12-15
        1.2.1 研究區(qū)域和對(duì)象 12-13
        1.2.2 研究方法和處理流程 13-14
        1.2.3 QUICKBIRD數(shù)據(jù)的特點(diǎn) 14-15
第2章 五大連池火山區(qū)的研究背景 15-21
    2.1 五大連池火山區(qū)的研究史 15-16
    2.2 五大連池火山區(qū)的構(gòu)造地質(zhì) 16
    2.3 五大連池火山區(qū)的火山地質(zhì) 16-18
    2.4 五大連池老黑山火山的熔巖 18-21
        2.4.1 老黑山噴出的結(jié)殼熔巖 18-19
        2.4.2 老黑山噴出的渣狀熔巖 19-21
第3章 老黑山西部熔巖流張裂的分布與特征 21-44
    3.1 張裂特征的野外觀察 21-22
    3.2 張裂的空間分布特征 22-41
        3.2.1 張裂的頻率分布 23-25
        3.2.2 張裂的組合特征 25-30
        3.2.3 張裂的優(yōu)勢(shì)方向特征 30-41
    3.3 熔巖穹丘的特征 41-44
第4章 五大連池老黑山西部熔巖流張裂的成因分析 44-49
    4.1 張裂的形成機(jī)制 44-46
    4.2 張裂的組合特征分析 46-48
    4.3 張裂的優(yōu)勢(shì)方向特征分析 48-49
結(jié)論 49-50
參考文獻(xiàn) 50-53
致謝 53-54

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