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研究生: Andrie Al Kausar
Andrie Al Kausar
論文名稱: 西至中爪哇第四紀火山岩之鋯石年代學與地球化學研究
Zircon U-Pb ages and geochemical characteristics of Quaternary volcanic rocks from West to Central Java
指導教授: 賴昱銘
Lai, Yu-Ming
口試委員: 賴昱銘
Lai, Yu-Ming
鍾孫霖
Chung, Sun-Lin
Iwan Setiawan
Iwan Setiawan
口試日期: 2022/06/06
學位類別: 碩士
Master
系所名稱: 地球科學系
Department of Earth Sciences
論文出版年: 2022
畢業學年度: 110
語文別: 英文
論文頁數: 125
中文關鍵詞: 鋯石U-Pb年齡地球化學火山岩西爪哇中爪哇
英文關鍵詞: Zircon U-Pb Ages, Geochemistry, Volcanic Rocks, West Java, Central Java
DOI URL: http://doi.org/10.6345/NTNU202200603
論文種類: 學術論文
相關次數: 點閱:87下載:10
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  • The Sunda Arc is located on the southeastern edge of Sundaland and was produced by the Indo-Australian Plate subduction of beneath the Eurasian Plate. Java Island is belonging to the eastern Sunda Arc, where arc magmatism began in the early Cenozoic and continued to Recent on this island. Previous studies used K-Ar methods for dating igneous rocks, which may easily to be affected by sample weathering and alteration. Furthermore, their geochemical analyses are limited to some prevalent volcanoes. In this work, I select six volcanic bodies in West Java and Central Java to study the zircon U-Pb geochronology and whole-rock geochemistry. A total of thirty-two volcanic rock samples were collected from West Java (Mount Sunda, Mount Malabar, Mount Guntur, and Mount Tangkuban) and Central Java (Mount Slamet and Mount Merapi). Geochemical compositions of these samples from West to Central Java range from calc-alkaline to high-K calc-alkaline with lithologies varying from basalt to andesite, and dacite. There are no significant variations among their Spidergram and Rare Earth Element (REE) patterns. They show the typical subduction signature which is enriched in Large Ion Lithophile Elements (LILE, Rb, Ba, Th, U, and K) and depleted in High Field Strength Elements (HFSE, Nb, Ta, and Ti) with negative Eu anomaly in some samples. Zircon U-Pb ages show that Mount Sunda erupted andesite (18JA03-1) and dacite (18JA03-4) around 4.0 Ma and 4.0 Ma, respectively. Mount Malabar erupted basaltic andesite (18JA04-1) and dacite (18JA05-1) yielding a mean age of 6.8 Ma and 4.4 Ma. Moreover, Mount Guntur basaltic andesite (17JA56) yield a mean age of 0.4 Ma. Both Mt. Slamet and Mt. Merapi samples are mafic and did not yield any zircon U-Pb age. According to the geochemical binary diagrams of major and trace elements from West Java, Mount Sunda and Tangkuban show characteristics of Rear-Arc while Mount Malabar is related to the Volcanic Front. Mount Guntur which shows transitional geochemical patterns indicate forming on the boundary between the Front Volcanic and Rear-Arc.

    CHAPTER 1. INTRODUCTION 1 1.1 General Introduction 1 1.2 Previous Studies 3 1.2.1 General Tectonics 3 1.2.2 Volcanism 8 1.2.3 Geochemistry and Age Dating 12 1.3 Aim and Motivation 13 CHAPTER 2. GEOLOGICAL BACKGROUND 15 2.1 Sunda Arc 15 2.2 Java 16 2.3 Regional Geology 20 2.3.1 Regional Geology of West Java 20 2.3.2 Regional Geology of Central Java 26 CHAPTER 3. METHODS AND SAMPLES 35 3.1 Methods 35 3.1.1 Petrography 35 3.1.2 Major and Trace Elements 36 3.1.3 Zircon U-Pb Dating 37 3.2 Samples 37 3.2.1 Mount Sunda 39 3.2.2 Mount Malabar 41 3.2.3 Mount Tangkuban 43 3.2.4 Mount Guntur 45 3.2.5 Mount Slamet 47 3.2.6 Mount Merapi 49 CHAPTER 4. RESULTS 53 4.1 Petrography 53 4.2 Geochemistry 54 4.2.1 Major Elements 54 4.2.2 Trace Elements 72 4.3 U-Pb Dating 77 CHAPTER 5. DISCUSSION 83 5.1 Typical Characteristics of Each Volcano 83 5.2 Magmatic Stages in West to Central Java during Cenozoic Era 88 5.3 The Geochemical Variations between VF and RA in West Java 93 CHAPTER 6. CONCLUSIONS 98 REFERENCES 99 APPENDICES 104 Appendices 1. Thin Section Photos 104 Appendices 2. CL-Images 116 Appendices 3. Zircon U-Pb Ages Results 119

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