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博碩士論文 etd-0908111-103829 詳細資訊
Title page for etd-0908111-103829
論文名稱
Title
柴北緣錫鐵山超高壓變質榴輝岩中綠輝石所含石英和角閃石析出物之成因
Origin of quartz and amphibole precipitates in omphacite in the ultrahigh-pressure metamorphosed eclogite from Xitieshan, North Qaidam
系所名稱
Department
畢業學年期
Year, semester
語文別
Language
學位類別
Degree
頁數
Number of pages
127
研究生
Author
指導教授
Advisor
召集委員
Convenor
口試委員
Advisory Committee
口試日期
Date of Exam
2011-07-04
繳交日期
Date of Submission
2011-09-08
關鍵字
Keywords
電子背向散射繞射、柴北緣超高壓變質帶、液包體、石英析出物、榴輝岩、綠輝石
North Qaidam ultrahigh-pressure metamorphism belt, fluid inclusion, quartz precipitates, omphacite, eclogite, electron backscattered diffraction
統計
Statistics
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The thesis/dissertation has been browsed 5699 times, has been downloaded 876 times.
中文摘要
在高壓-超高壓變質帶的榴輝岩或石榴石橄欖岩中,常可見到斜輝石中含有順向排列的針狀或棒狀之石英析出物,此種現象常被用來當作該岩石經歷過超高壓變質作用的一種指標,然而關於這種石英析出物的成因以及它們和斜輝石主晶之間是否有結晶構造上的特定方位關係仍然不是很清楚。為了探討石英析出物的形成機制、生成環境,本研究利用電子背向散射繞射(electron backscattered diffraction, EBSD)分析、岩象觀察和礦物成份分析來研究柴北緣超高壓變質帶錫鐵山之榴輝岩中的綠輝石所含之石英與角閃石析出物,分析其岩象特徵、礦物組合、礦物成份以及綠輝石與所含析出物之結晶方位關係。研究結果顯示綠輝石所含順向排列之棒狀析出物主要為石英 ± 淡閃石的組合,析出物長約 5 ~ 20 &micro;m,寬約 3 ~ 8 &micro;m,其長軸方向與主晶綠輝石c軸方向大致平行,且析出物常呈現綠輝石主晶的負晶體外形。由EBSD的分析結果顯示淡閃石和石英析出物分別與綠輝石主晶呈現結晶順構關係,淡閃石的a, b, c軸分別和綠輝石a, b, c軸一致。而石英析出物與主晶綠輝石亦呈現兩組主要的結晶順構關係,第一組石英析出物的長軸為a軸,a Qtz // c Omp,c Qtz ~// <201>Omp,{0001} Qtz // {100}Omp;第二組石英析出物的長軸為c軸,c Qtz // cOmp,a Qtz ~// <201>Omp,{21 &#773;1 &#773;0} Qtz // {100}Omp;兩組石英析出物方位的a-c面均平行綠輝石的a-c面,即{011 &#773;0} Qtz // {010}Omp。根據此石英 ± 淡閃石析出物所具有的負晶組織特徵,推測錫鐵山榴輝岩綠輝石在峰期變質之後的退變階段離溶出液包體,此液包體提供了石英和淡閃石析出物的生長空間與部份材料,析出物在成長的過程中,為了維持最小之晶界界面能,分別呈現主晶和析出物之間的結晶順構關係。彙整前人研究斜輝石析出石英 ± 角閃石的資料顯示,高壓-超高壓變質岩中的斜輝石含有石英 ± 角閃石析出物者,大都有經歷過高壓粒變岩相的疊加作用,意味著溫度可能才是析出物產出的關鍵因素,而非一般認為的壓力因素。因此,綠輝石含石英 ± 角閃石析出物,不適合當作岩體經歷過超高壓變質作用的指標。
Abstract
Oriented needle-shaped or rod-shaped quartz precipitates occur in clinopyroxenes have been commonly observed in eclogites or garnet peridotites from the high pressure or ultra-high pressure (HP/UHP) metamorphic belts, and their occurrence has been used as an indicator of UHP metamorphism. However, the origin of those quartz precipitates and their crystallographic orientation relationships with clinopyroxene hosts are still not clear. In order to understand the formation mechanisms and environments of the quartz precipitates, the present study has used electron backscattered diffraction (EBSD) analysis, petrographic and scanning electron microscopy, and electron microprobe analysis to study textural features, mineral assemblages, mineral compositions, and crystallographic orientation relationships of mineral precipitates in the omphacite from Xitieshan, North Qaidam UHP metamorphic belt. The results show that the oriented rod-like precipitates in the omphacite hosts are mainly composed of quartz + edenite, and the rods are 5~20
目次 Table of Contents
論文審定書………………………………….……………………………...……… i
誌謝辭……………………………………………………………………………… ii
中文摘要……………………………………………………………………….….. iii
英文摘要……………………………………………………...…………...………. v
目錄…………………………………………………………..….………………. vii
圖目錄…………………..………………………………………….…………. ix
表目錄…………………..……………………………………………….………. xii
礦物符號縮寫表………………………………………….…..……………...…. xiii

第一章 序論……………………………………………………………..…...….. 1
1-1 前言…..…..………………………………….………………...…..…… 1
1-2 前人研究………..…………………………………...………….....…… 4
1-3 研究動機與目的…….…..…………………………………….......…… 6
第二章 地質背景……………………………..………………………...…..…… 8
2-1 柴北緣超高壓變質帶..………….…………………….…………...…… 8
2-1-1 地體演化..………………………………..……………....…… 8
2-1-2 柴北緣地體經歷超高壓變質的證據……………………......… 9
2-1-3 溫度-壓力路徑…………………..….……….……………… 10
2-2 研究樣品…………………………………….………………….............. 11
第三章 研究方法……………………………..………………………….……… 15
3-1 實驗流程……………………….…..…………………....….…...……… 15
3-2 實驗方法與儀器..………………………………………….……....…… 16
3-2-1 偏光顯微鏡之岩象觀察.……………….……………….……… 16
3-2-2 SEM/EDS之觀察與成份分析……….……………….……..… 16
3-2-3 EBSD之結晶方位鑑定……….……….…………….……..… 17
3-3 岩石光薄片製備…..………………………………………….…...…... 19
3-3-1 SEM/EDS之岩石光薄片製備方式…………………….……... 19
3-3-2 EBSD之岩石光薄片製備方式……….………………………... 19
3-3-3 EBSD之結晶方位鑑定………...……………….…….………... 18
3-4 礦物成份之計算與繪圖………………………………….….………..... 20
3-4-1 輝石成份計算與投圖……………….…………………..…..... 20
3-4-2 角閃石成份計算與投圖............................................................... 23
3-4-3 其它常見礦物成份計算............................................................. 28
第四章 結果…………………………………..………………………………… 29
4-1 標本觀察…………………………………………………………….… 29
4-2 岩象觀察與SEM/EDS成份分析……………………………..……… 31
4-2-1 魚卡河(YKH)榴輝岩……………………………………… 31
4-2-2 錫鐵山(XTS)榴輝岩……………………………..………… 33
4-3 錫鐵山綠輝石所含析出物之觀察………………………..…...……… 54
4-3-1 針狀/棒狀的負晶體外形之石英 ± 淡閃石析出物…..…...... 54
4-3-2 條帶狀的淡閃石析出物……………………………..…...…. 55
4-3-3 疑似鈉長石的析出物………………………………..…...…. 55
4-4 錫鐵山榴輝岩綠輝石與所含析出物之結晶方位鑑定……………….. 60
4-4-1 EBSD結晶方位鑑定……………………………………..…… 60
4-4-2 綠輝石與負晶形石英析出物之結晶方位關係……………...… 63
第五章 討論………………………………………………......................……… 88
5-1 綠輝石中所含棒狀析出物之組成與組織特徵……………………..… 88
5-2 綠輝石與析出物的結晶順構關係………………………………...… 89
5-3 綠輝石所含析出物的生長機制……………………………………...… 90
5-3-1 負晶形析出物與液包體之關聯性…………………………...… 90
5-3-2 礦物反應與離溶作用………………………………………...… 93
5-4 綠輝石所含析出物之生長環境……………………………………...… 94
5-5 錫鐵山榴輝岩與所含石英 ± 淡閃石析出物之生長條件與過程…… 96
第六章 結論……………………………………………...........................…… 101
參考文獻…………………………………….......……………………………… 103
參考文獻 References
英文文獻
Anderson, E. D., Moecher, D. P. (2007) Omphacite breakdown reactions and relation to eclogite exhumation rates. Contributions to Mineralogy and Petrology, 154, 253-277.
Boschmann, K. F., Burns, P. C., Hawthorne, F. C. (1994) A-site disorder in synthetic fluor-edenite, a crystal structure study. Canadian Mineralogist, 32, 21-30.
Chopin, C. (1984) Coesite and pure pyrope in high-grade blueschists of the Western Alps: a first record and some consequences. Contributions to Mineralogy and Petrology, 86, 107-118.
Coleman, R. G., Lee, D. E., Beatty, L. B., Brannock, W. W. (1965) Eclogites and Eclogites: Their Differences and Similarities. Geological Society of America Bulletin, 76, 483-508.
Deer, W. A., Howie, R. A., Zussman, J. (1992) An Introduction to theRock-Forming Minerals ( 2nd edition ). Prentice Hall, 696pp.
Dobrzhinetskaya, L. F., Schweinehage, R., Massonne, H. J., Green, H. W. (2002) Silica precipitates in omphacite from eclogite at Alpe Arami, Switzerland: evidence of deep subduction. Journal of Metamorphic Geology, 20, 481-492.
Droop, G. T. R. (1987) A general equation for estimating Fe3+ concentrations in ferromagnesian silicates and oxides from microprobe analyses, using stoichiometric criteria. Mineralogical Magazine, 51, 431-4350.
Ernst, W. G. (2001) Subduction, ultrahigh-pressure metamorphism, and regurgitation of buoyant crustal slices - implications for arcs and continental growth. Physics of the Earth and Planetary Interiors, 127, 253-275.
Ernst, W. G., Liou, J. G. (2008) High- and ultrahigh-pressure metamorphism: Past results and future prospects. American Mineralogist, 93, 1771-1786.
Feinberg, J. M., Wenk, H. R., Renne, P. R., Scott, G. R. (2004) Epitaxial relationships of clinopyroxene-hosted magnetite determined using electron backscatter diffraction (EBSD) technique. American Mineralogist, 89, 462–466.
Gottesmann, B., Wirth, R. (1997) Pyrrhotite inclusion in dark pigmented apatite from granitic rock. European Journal of Mineralogy, 9, 491–500.
Hwang, S. L., Shen, P., Chu, H. T., Yui, T. F., Liou, J. G., Sobolev, N. V. (2009) Kumdykolite, an orthorhombic polymorph of albite, from the Kokchetav ultrahigh-pressure massif, Kazakhstan. European Journal of Mineralogy, 21, 1325-1324.
Hwang, S. L., Shen, P., Chu, H. T., Yui, T. F. (2010) On the coherency-controlled growth habit of precipitates in minerals. Journal of Applied Crystallography, 43, 417-428.
Katayama, I., Parkinson C. D., Okamoto, K., Nakajima, Y., Maruyama, S. (2000) Supersilicic clinopyroxene and silica exsolution in UHPM eclogite and pelitic gneiss from the Kokchetav massif, Kazakhstan. American Mineralogist, 85, 1368-1374.
Konzett, J., Libowitzky, E., Hejny, C., Miller, C., Zanetti, A. (2008a) Oriented quartz+calcic amphibole inclusions in omphacite from the Saualpe and Pohorje Mountain eclogites, Eastern Alps-An assessment of possible formation mechanisms based on IR- and mineral chemical data and water storage in Eastern Alpine eclogites. Lithos, 106, 336-350.
Konzett, J., Frost, D. J., Proyer, A., Ulmer, P. (2008b) The Ca-Eskola component in eclogitic clinopyroxene as a function of pressure, temperature and bulk composition: an experimental study to 15 GPa with possible implications for the formation of oriented SiO2-inclusions in omphacite. Contributions to Mineralogy and Petrology, 155, 215-228.
Lager, G. A., Jorgensen, J. D., Rotella, F. J. (1982) Crystal structure and thermal expansion of α&#8208;quartz SiO2 at low temperatures. AIP Conference Proceedings, 89, 75-77.
Leake, B. E., Woolley, A. R., Arps, C. E. S., Birch, W. D., Gilbert, M. C., Grice, J. D., Hawthorne, F. C., Kato, A., Kisch, H. J., Krivovichev, V. G., Linthout, K., Laird, J., Mandarino, J. A., Maresch, W. V., Nickel, E. H., Rock, N. M. S., Schumacher, J. C., Smith, D. C., Stephenson, N. C. N., Whittaker, E. J. W., Youzhi, G. (1997) Nomenclature of amphiboles: report of the subcommittee on amphiboles of the International Mineralogical Association, Commission on New Minerals and Mineral Names. The Canadian Mineralogist, 35, 219-246.
Liou, J. G., Zhang, R. Y., Ernst, W. G., Rumble, D., Maruyama, S. (1998) High-pressure minerals from deeply subducted metamorphic rocks. In: Hemley, R. J. (ed.) Ultrahigh-pressure mineralogy: physics and chemistry of the Earth's deep interior, Reviews in Mineralogy. Mineralogical Society of America, 37, 33-96.
Liou, J. G., Tsujimori, T., Zhang, R. Y., Katayama, I., Maruyama, S. (2004) Global UHP metamorphism and continent subduction/collision: the Himalayan model. International Geology Review, 46, 1-27.
Liou, J. G., Ernst, W. G., Zhang, R. Y., Tsujimori, T., Jahn, B. M. (2009) Ultrahigh-pressure minerals and metamorphic terranes - The view from China. Journal of Asian Earth Sciences, 35, 199-231.
Mao, H. K. (1971) The system jadeite (NaAlSi2O6) - anorthite (CaAl2Si2O8) at high pressures. Carnegie Institution Year Book, 69, 163–168.
Morimoto, N. (1988) Nomenclature of pyroxenes. Mineralogical Magazine, 52, 535-550.
Nakano, N., Osanai, Y., Owada, M. (2007) Multiple breakdown and chemical equilibrium of silicic clinopyroxene under extreme metamorphic conditions in the Kontum Massif, central Vietnam. American Mineralogist, 92, 1844-1855.
Oberti, R., Caporuscio, F. A. (1991) Crystal chemistry of clinopyroxenes from mantle eclogites: A study of the key role of the M2 site population by means of crystal - structure refinement. American Mineralogist, 76, 1141-1152.
Ogasawara, Y., Fukasawa, K., Maruyama, S. (2002) Coesite exsolution from supersilicic titanite in UHP marble from the Kokchetav Massif,northern Kazakhstan. American Mineralogist, 87, 454-461.
Page, F. Z., Essene, E. J., Mukasa, S. B. (2005) Quartz exsolution in clinopyroxene is not proof of ultrahigh pressures: Evidence from eclogites from the Eastern Blue Ridge, Southern Appalachians, U.S.A. American Mineralogist, 90, 1092-1099.
Proyer, A., Krenn K., Hoinkes G.. (2009) Oriented precipitates of quartz and amphibole in clinopyroxene of metabasites from the Greek Rhodope: a product of open system precipitation during eclogite–granulite–amphibolite transition. Journal of Metamorphic Geology, 27, 639-654.
Roedder, E. (1984) Fluid Inclusions, Reviews in Mineralogy, 12. Mineralogical Society of America, 646 p.
Sajeev, K., Kawai, T., Omori, S., Windley, B. F., Maruyama, S. (2010) P - T evolution of Glenelg eclogites, NW Scotland: Did they experience ultrahigh-pressure metamorphism? Lithos, 114, 473-489.
Seto, Y., Ohi, S., Shimobayashi, N., Kitamura, M., Miyake, A., Hiroi. Y., Grantham, G.H. (2006) Clinopyroxene exsolution in wollastonite from Namaqualand granulite, South Africa. American Mineralogist, 91, 446–450.
Schmadicke, K., Muller, W. F. (2000) Unsual exsolution phenomena in omphacite and partial replacement of phengite by phlogopite + kyanite in an eclogite from the Erzgebirge. Contributions to Minerology and Petrology, 139, 629-642.
Shau. Y. H., Tsai, H. G., Liu, Y. H., Yu, S. C., Yang, J., Xu, C. (2005) Transmission electron microscopic study of quartz rods with intergrown amphibole within omphacite in eclogites from the Sulu ultrahigh-pressure metamorphic terrane, eastern China. 7th Internationl Eclogite Conference Abstracts. Mitteilungen der &Ouml;sterreichischen Mineralogischen Gesellschaft, 150, 139.
Smith, D. C. (1984) Coesite in clinopyroxene in the Caledonides and its implications for geodynamics. Nature, 310, 641-644.
Song, S. G., Zhang, L. F., Niu, Y. L., Su, L., Jian, P., Liu, D. (2005a) Geochronology of diamond-bearing zircons from garnet peridotite in the North Qaidam UHPM belt, Northern Tibetan Plateau: A record of complex histories from oceanic lithosphere subduction to continental collision . Earth and Planetary Science Letters, 234, 99–118.
Song, S. G., Zhang, L. F., Chen, J., Liou, J. G., Niu, Y. L. (2005b) Sodic amphibole exsolutions in garnet from garnet - peridotite, North Qaidam UHPM belt, NW China: Implications for ultradeep - origin and hydroxyl defects in mantle garnets. American Mineralogist, 90, 814–820.
Stout, J. H. (1972) Phase petrology and mineral chemistry of coexisting amphiboles from Telemark, Norway. Journal of Petrology, 13, 99-145.
Sturm, R. (2002) PX - NOM – an interactive spreadsheet program for the computation of pyroxene analyses derived from the electron microprobe. Computers and Geosciences, 28, 473-483.
Tindle, A. G., Webb, P.C. (1994) PROBE-AMPH – a spreadsheet program to classify microprobe - derived amphibole analyses. Computers & Geosciences, 20, 1201-1228.
Tsai, C. H., Liou, J. G. (2000) Eclogite-facies relies and inferred ultrahighpressure metamorphism in the North Dabie Complex, Central - eastern China. American Mineralogist, 85, 1-8.
Wilkins, R. W. T. (1977) The role of fluid inclusions in the exsolution of clinopyroxene in bustamite from Broken Hill, New South Wales. Australia. American Mineralogist, 62, 465-474.
Yamamoto, S., Komiya, T., Hirose, K., Maruyama, S. (2009) Coesite and clinopyroxene exsolution lamellae in chromites: In-situ ultrahigh-pressure evidence from podiform chromitites in the Luobusa ophiolite, southern Tibet. Lithos, 109, 314–322.
Yang, J. S., Xu, Z. Q., Song, S. G., Zhang, J. X., Wu, C. L., Shi R. D., Li, H. B., Brunel, M. (2001) Discovery of coesite in the North QaidamEarly Palaeozoic ultrahigh pressure (UHP) metamorphic belt, NW China. Earth and Planetary Sciences, 333, 719-724.
Zhang, C., Zhang, L. F.., Roermund, H. V., Song, S. G., Zhang, G. B. (2011) Petrology and SHRIMP U–Pb dating of Xitieshan eclogite, North Qaidam UHP metamorphic belt, NW China. Journal of Asian Earth Sciences. in Press.
Zhang, G. B., Ellis, D. J., Christy, A. G., Zhang, L. F., Niu, Y. L., Song, S. G. (2009) UHP metamorphic evolution of coesite - bearing eclogite from the Yuka terrane, North Qaidam UHPM belt, NW China: Petrological and isotopic constraints. European Journal of Mineralogy, 21, 1287-1300.
Zhang, J. X., Yang, J. S., Mattinson, C. G., Xu, Z. Q., Meng, F. C., Shi, R. D. (2005) Two contrasting eclogite cooling histories, North Qaidam HP/UHP terrane, western China: Petrological and isotopic constraints. Lithos, 84, 51-76.
Zhang, L. F., Ellis, D. J., Jiang, W. B. (2002) Ultrahigh - pressure metamorphism in western Tianshan, China: Part I. Evidence from inclusions of coesite pseudomorphs in garnet and from quartz exsolution lamellae in omphacite in eclogites. American Mineralogist, 87, 853-860.
Zhang, L. F., Song, S. G., Liou, J. G., Ai, Y. L., Li, X. P. (2005) Relict coesite exsolution in omphacite from Western Tianshan eclogites, China. American Mineralogist, 90, 181-186.
Zhang, R. Y., Zhai, S. M., Fei, Y. W., Liou, J. G. (2003) Titanium solubility in coexisting garnet and clinopyroxene at very high pressure: the significance of exsolved rutile in garnet. Earth and Planetary Science Letters, 216, 591-601.
Zhang, Z. M., Shen, K., Liou, J. G., Zhao, X. D. (2007) Fluid inclusion associated with exsolved quartz needles in omphacite of UHP eclogites, Chinese Continental Scientific Drilling Main Drillhole. International Geology Review, 49, 479-486.
Zhu, Y., Ogasawara, Y. (2002) Phlogopite and Coesite Exsolution from Super-Silicic Clinopyroxene. International Geology Review, 44, 831-836.

中文文獻
王 璐、金振民、何謀春(2003)榴輝岩中石英出溶體的拉曼光譜學研究及其構造意義。地球科學-中國地質大學學報,第28卷,第2期,143-150頁。
王清海、許文良、王冬豔、林景仟、劉曉春(2002)徐淮地區鎂鐵質岩石捕虜体單斜輝石中石榴石和石英的出溶。高校地質學報,第8卷,第4期,407-415頁。
王惠初、袁桂邦、辛后田、郝國傑、鄭健康、張寶華(2001)柴北緣綠梁山地區榴輝岩的產狀及其成因意義初探。中國地質,第28卷,第7期,22-28頁。
朱永峰、Massonne, H. J.(2005)磷灰石中磁黃鐵礦出溶結構的發現。岩石學報,第21卷,第2期,第405-410頁。
朱孟番、朱永峰(2007)蘇魯三清閣榴輝岩中柯石英的發現及其地質意義探討。高校地質學報,第13卷,第3期,第581-589頁。
宋述光、張立飛、Niu, Y.、宋 彪、劉墩一(2004)青藏高原北緣早古生代板塊構造演化和大陸深俯衝。地質通報,第23卷,第9~10期,第918-925頁。
孟繁聰、張建新、楊經綏(2005)柴北緣錫鐵山古生代HP/UHP變質作用後的構造熱事件-花崗岩和片麻岩的同位素與岩石地球化學證據。岩石學報,第21卷,第1期,第45-56頁。
夏瓊霞、鄭永飛(2011)高壓-超高壓變質岩石中石榴石的環帶和成因。岩石學報,第27卷,第2期,第433-450頁。
孫 賀、肖益林(2009)流體包裹體研究:進展、地質應用及展望。地球科學進展,第24卷,第10期,第1105-1121頁。
婁玉行、魏春景、初 航、王 偉、張景森(2009)西大別造山帶紅安高壓榴輝岩的變質演化:岩相學與Na2O–CaO–K2O–MgO–Al2O3–SiO2–H2O–
O(Fe2O3 )體系中相平衡關系。岩石學報,第25卷,第1期,第124-138頁。
張 聰、張立飛、張貴賓、宋述光(2009)柴北緣錫鐵山一帶榴輝岩的岩石學特徵及其退變PT軌跡。岩石學報,第25卷,第9期,2247-2259頁。
張建新、孟繁聰、楊經綏(2005)柴北緣魚卡榴輝岩的pT演化歷史。岩石礦物學雜誌,第24卷,第4期,245-254頁。
張建新、孟繁聰、李金平(2009)柴達木北緣榴輝岩中的柯石英及其意義。科學通報,第54卷,第5期,618-623頁。
楊經綏、許志琴、李海兵、吳才來、崔軍文、張建新、陳 文(1998)我國西部柴北緣地區發現榴輝岩。科學通報,第43卷,第14期,第1544-1549頁。
楊經綏、許志琴、宋述光、吳才來、史仁燈、張建新、萬渝生、李海兵、金小赤、Jolivet, M.(2000)青海都蘭榴輝岩的發現及對中國中央造山帶內高壓─超高壓變質帶研究的意義。地質學報,第74卷,第2期,156-168頁。
楊經綏、宋述光、許志琴、吳才來、史仁燈、張建新、李海兵、萬渝生、劉 焰、邱海峻、劉福來、Maruyama, S.(2001)柴達木盆北緣早古生代高壓-超高壓變質帶中發現典型超高壓礦物-柯石英。地質學報,第75卷,第2期,,175-179頁。
楊經綏、許志琴、張建新、張澤明、劉福來、吳才來(2009)中國主要高壓-超高壓變質帶的大地構造背景及俯衝/折返機制的探討。岩石學報,第25卷,第7期,第1529-1560頁。
張建新、孟繁聰、戚學祥(2002)柴達木盆地北緣大柴旦和錫鐵山榴輝岩中石榴子石環帶對比及地質意義。地質通報,第21卷,第3期,123-129頁。
張建新、孟繁聰、C. G. Mattinson(2007)南阿爾金─柴北緣高壓-超高壓變質帶研究進展、問題及挑戰。高校地質學報,第13卷,第3期,526-545頁。
張建新、於勝堯、孟繁聰(2008)柴達木北緣魚卡-落鳳坡榴輝岩-片麻岩單元的變質變形演化。地質通報,第27卷,第9期,1468-1474頁。
張澤明、沈昆、趙旭東、石超(2006)超高壓變質作用過程中的流體—來自蘇魯超高壓變質岩岩石學、氧同位素和流體包裹體研究的限定。岩石學報,第22卷,第7期,第1985-1998頁。
梁金龍、孫曉明、徐 莉、翟 偉、湯 倩、梁業?琚]2006)CCSD超高壓變質岩綠輝石中的石英出溶體及其大陸動力學意義。地質學報,第80卷,第12期,第1904-1910頁。
章軍鋒、金振民、Green, H. W.、金淑燕(2000)大陸深俯衝帶中的水:來自大別山超高壓榴輝岩的證據。科學通報,第45卷,第17期,第1889-1894頁。
許志琴、楊經綏、吳才來、李海兵、張建新、戚學祥、宋述光、萬渝生、陳 文、邱海峻(2003)柴達木北緣超高壓變質帶形成與折返的時限及機制。地質學報,第77卷,第2期,第164-176頁。
郭妍伶(2009)北大別山石榴單輝岩中析出物與離溶片晶之研究。國立東華大學地球科學研究所碩士論文,197頁。
陳丹玲、孫 勇、劉 良、張安達、羅金海、王 焰(2005)柴北緣魚卡河榴輝岩的變質演化-石榴石成分環帶及礦物反應結構的證據。岩石學報,第21卷,第4期,1039-1048頁。
陸松年、王惠初、李懷坤、袁桂邦、辛後田、鄭健康(2002)柴達木盆地北緣“達肯大阪群”的再厘定。地質通報,第21卷,第1期,第19-23頁。
湯 倩(2005)礦物中的包裹體及其研究意義。中山大學研究生學刊(自然科學、醫學版),第26卷,第3期,第75-84頁。
黃宏勝、吳美倫、林麗娟(2006)EBSD應用在低溫多晶矽薄膜之微結構分析與研究。工業材料雜誌,第238期,第174-180頁。
劉俊來、曹淑雲、鄒運鑫、宋志傑(2008)岩石電子背散射衍射(EBSD)組構分析及應用。地質通報,第26卷,第10期,第1638-1645頁。
劉祥文、金振民、曲 晶、王 璐(2005)石榴石異剝橄欖岩中橄欖石的鈦鐵礦和含鉻鈦鐵礦出溶體。中國科學D輯-地球科學,第35卷,第10期,第949-956頁。
蔡宗翰(2005)中國南蘇&#63801;地區隕&#63950;鐵(磁黃鐵礦)於磷灰石中之結晶關係研究。國&#63991;成功大學地球科學研究所碩士&#63809;文,103頁。
蔡憲璋(2006)中國蘇&#63801;超高壓變質帶東海地區榴輝岩之礦物析出物研究。國&#63991;中山大學海洋生物科技暨資源學系碩士班碩士論文,135頁。
蘇 文、游振東、王汝成、劉祥文(2001)大別山北部石榴輝石巖透輝石中石英和單斜頑火輝石的出溶。科學通報,第46卷,第10期,第850-854頁。
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