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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 施路易(Ludvig Lowemark) | |
| dc.contributor.author | Weng-Si Chao | en |
| dc.contributor.author | 周穎詩 | zh_TW |
| dc.date.accessioned | 2021-06-16T09:50:51Z | - |
| dc.date.available | 2017-02-16 | |
| dc.date.copyright | 2017-02-16 | |
| dc.date.issued | 2017 | |
| dc.date.submitted | 2017-01-17 | |
| dc.identifier.citation | Adler, R.E., Polyak, L., Ortiz, J.D., Kaufman, D.S., Channell, J.E.T., Xuan, C., Grottoli, A.G., Sellén, E. and Crawford, K.A., 2009. Sediment record from the western Arctic Ocean with an improved Late Quaternary age resolution: HOTRAX core HLY0503-8JPC, Mendeleev Ridge. Global and Planetary Change, 68(1–2): 18-29.
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/60017 | - |
| dc.description.abstract | The sediment deposited in the Arctic Ocean is transported by sea ice and icebergs, which are controlled by the Arctic surface circulations. Several cores from the central
Arctic, the Lomonosov Ridge north of Greenland and the Morris Jesup Rise contain a distinct grayish, ice rafted debris (IRD)-rich, layer with some specific features: a sharp lower boundary, relatively low content of manganese, and a lack of bioturbation. Heavy minerals from these layers were analyzed primarily by Electron Probe X-Ray Microanalyzer (EPMA) and Scanning Electron Microscope-Energy Dispersive Spectrometer (SEM-EDS) to establish the prominent provenance areas. The provenance variations can show the paleo-distribution and transport pathways of sea ice and icebergs and even indicate the origin of some abrupt glacial events. Initial results suggest that the majority of the grains in the gray layer originated from a limited area near the Putorana Basalt Plateau. We therefore hypothesize that this gray layer is related to an abrupt ice dammed lake drainage from northern Siberia, tentatively dated to around the boundary between MIS 4 and 3 based on all available chronostratigraphic data points and the correlation of distinct geochemical and sedimentological features: variation in Mn, bulk density, bioturbation and abundance of planktonic and benthic foraminifera; including published data and measured data in this study. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-16T09:50:51Z (GMT). No. of bitstreams: 1 ntu-106-R03224215-1.pdf: 11687567 bytes, checksum: cb5ffae2f439b7d431cd9c7dda6f3909 (MD5) Previous issue date: 2017 | en |
| dc.description.tableofcontents | 致謝 ................................................................................................................................... I
中文摘要 .......................................................................................................................... II Abstract............................................................................................................................ III Contents............................................................................................................................ V List of Figures................................................................................................................. VII List of Tables ................................................................................................................... IX CHAPTER 1 - Objectives ................................................................................................ 1 CHAPTER 2 - Background .............................................................................................. 4 2.1 Geography .......................................................................................................... 4 2.2 Hydrology and sedimentary processes ............................................................... 6 2.3 Geology of Arctic surrounding landmasses........................................................ 7 2.4 Rivers input and manganese cycle...................................................................... 9 2.5 Ice sheet history................................................................................................ 10 2.6 Gray IRD-rich layer.......................................................................................... 12 2.7 Ice dammed lakes and outbursts....................................................................... 13 CHAPTER 3 – Materials and methods........................................................................... 15 3.1 Core material .................................................................................................... 15 3.2 X-ray radiographs ............................................................................................. 18 3.3 XRF analysis - ITRAX core scanner................................................................ 20 3.4 Heavy mineral analysis..................................................................................... 21 3.4.1 Heavy mineral study.............................................................................. 21 3.4.2 Sample selection and preparation .......................................................... 23 3.4.3 Heavy mineral separation ...................................................................... 25 3.4.4 Electron microprobe analysis ................................................................ 29VI 3.5 Data processing ................................................................................................ 33 3.5.1 Sorting in Excel ..................................................................................... 33 3.5.2 MinIdent-Win 4.0 software ................................................................... 35 CHAPTER 4 – Result..................................................................................................... 36 4.1 Digital photography.......................................................................................... 36 4.2 Radiograph and trace fossil .............................................................................. 38 4.3 XRF result ........................................................................................................ 45 4.4 EPMA result ..................................................................................................... 49 CHAPTER 5 – Discussion ............................................................................................. 58 5.1 Methodology..................................................................................................... 58 5.1.1 Heavy mineral separation method ......................................................... 58 5.1.2 Minerals cleaning .................................................................................. 59 5.1.3 Sample surface....................................................................................... 60 5.1.4 Sampling points and total number for measurement ............................. 61 5.2 Excel sorting vs. MindIdent-Win 4.0 ............................................................... 62 5.3 Age control and core correlation ...................................................................... 67 5.4 The IRD-rich gray layer and interpretation ...................................................... 70 CHAPTER 6 – Conclusion............................................................................................. 82 References ...................................................................................................................... 84 Appendix A..................................................................................................................... 90 Appendix B................................................................................................................... 106 | |
| dc.language.iso | en | |
| dc.subject | 來源 | zh_TW |
| dc.subject | 沉積學 | zh_TW |
| dc.subject | 錳 | zh_TW |
| dc.subject | 重礦物 | zh_TW |
| dc.subject | 生物擾動 | zh_TW |
| dc.subject | 灰色沉積層 | zh_TW |
| dc.subject | 北極海 | zh_TW |
| dc.subject | Heavy mineral | en |
| dc.subject | Manganese | en |
| dc.subject | Bioturbation | en |
| dc.subject | Gray layer | en |
| dc.subject | Provenance | en |
| dc.subject | Sedimentology | en |
| dc.subject | Arctic Ocean | en |
| dc.title | 格陵蘭外海羅蒙諾索夫海脊上獨特灰色沉積層之來源探討 | zh_TW |
| dc.title | Heavy Mineral Provenance of a Distinct Gray Layer from the Lomonosov Ridge off Greenland | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 105-1 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 黃國芳(Kuo-Fang Huang),飯塚義之(Yoshiyuki Iizuka),蘇志杰(CHIH-CHIEH SU) | |
| dc.subject.keyword | 北極海,重礦物,來源,灰色沉積層,生物擾動,錳,沉積學, | zh_TW |
| dc.subject.keyword | Arctic Ocean,Heavy mineral,Provenance,Gray layer,Bioturbation,Manganese,Sedimentology, | en |
| dc.relation.page | 106 | |
| dc.identifier.doi | 10.6342/NTU201700098 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2017-01-17 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 地質科學研究所 | zh_TW |
| 顯示於系所單位： | 地質科學系 | |
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