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Shi wan lao ren yi men shi jie
No full text張璐纂述 ; [張]登, [張]倬參訂.綫裝.框18.9x12.9公分, 9行20字. 白口, 四周雙邊, 無魚尾. 版心上鐫"醫通"及卷次, 中鐫小題, 下鐫葉次.卷首附《引用書目》及《石頑老人醫門十戒》書名頁刻"張氏醫通, 吳門張路玉先生纂述, 千金方衍義嗣出, 寳翰樓梓"前有康熙三十二年[1693]汝湖序, 三十四年[1695]自序, 四十八年[1709]朱彜尊序. 又有四十四年[1705]張以柔進醫通疏, 言此書已刊版行世.《中國中醫古籍總目》05639著錄有清康熙四十八年寳翰樓刻本. 《中國叢書綜錄》(p.721)著錄《張氏醫書七種》, 清康熙寳翰樓刻本, 收此零種.鈐"張氏藏書", "徐氏稚鴻", "稚鴻", "稚鴻藏書", "莊兆祥印".Xian zhuang.Kuang 18.9 x 12.9 gong fen, 9 hang 20 zi. Bai kou, si zhou shuang bian, wu yu wei. Ban xin shang juan "Yi tong" ji juan ci, zhong juan xiao ti, xia juan ye ci.Detailed notes in vernacular field only.Detailed notes in vernacular field only.Detailed notes in vernacular field only.Detailed notes in vernacular field only.Zhang Lu zuan shu ; [Zhang] Deng, [Zhang] Zhuo can ding.Qian "Zhang shi cang shu", "Xu shi Zhihong", "Zhihong", "Zhihong cang shu", "Zhuang Zhaoxiang yin"
Going Beyond Counting First Authors in Author Co-citation Analysis
Get PDFThe present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation
counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings
are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that
only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into
account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed
Variations on the Author
Get PDF“Variations on the Author” discusses two of Eduardo Coutinho’s recent films (Um Dia na Vida, from 2010, and Últimas Conversas, posthumously released in 2015) and their contribution to the general question of documentary authorship. The director’s filmography is characterized by a consistent yet self-effacing form of authorial self-inscription: Coutinho often features as an interviewer that rather than express opinions propels discourses; an interviewer that is good at listening. This mode of self-inscription characterizes him as an author who is not expressive but who is nonetheless markedly present on the screen. In Um Dia na Vida, however, Coutinho is completely absent form the image, while Últimas Conversas, on the contrary, includes a confessional prologue that moves the director from the margins to the center of his films. This article examines the ways in which these works stand out in the filmography of a director who offers new insights into the notion of cinematic authorship
Appropriate Similarity Measures for Author Cocitation Analysis
Get PDFWe provide a number of new insights into the methodological discussion about author cocitation analysis. We first argue that the use of the Pearson correlation for measuring the similarity between authors’ cocitation profiles is not very satisfactory. We then discuss what kind of similarity measures may be used as an alternative to the Pearson correlation. We consider three similarity measures in particular. One is the well-known cosine. The other two similarity measures have not been used before in the bibliometric literature. Finally, we show by means of an example that our findings have a high practical relevance.information science;Pearson correlation;cosine;similarity measure;author cocitation analysis
Dispelling the Myths Behind First-author Citation Counts
Get PDFWe conducted a full-scale evaluative citation analysis study of scholars in the XML research field to explore just how different from each other author rankings resulting from different citation counting methods actually are, and to demonstrate the capability of emerging data and tools on the Web in supporting more realistic citation counting methods. Our results contest some common arguments for the continued
use of first-author citation counts in the evaluation of scholars, such as high correlations between author rankings by first-author citation counts and other citation
counting methods, and high costs of using more realistic citation counting methods that are not well-supported by the ISI databases. It is argued that increasingly available digital full text research papers make it possible for citation analysis studies to go beyond what the ISI databases have directly supported and to employ more
sophisticated methods
Sedimentation and Evolution of Kaoping Slope Basin and Penghu Submarine Canyon-Channel System off Southwest Taiwan
No full text摘要
現今臺灣西南海域可視為臺灣西部前陸盆地系統向西南延伸的楔形體上方堆積區（wedge top depozone），也是未充填滿的初期前陸盆地（underfilled foreland basin）。上新世以來，來自臺灣造山帶線來源（line source）及點來源（point source）的沈積物，分別經由向海加積的方式及海底峽谷輸送管道，將沈積物輸送到西南前陸盆地堆積。高屏陸棚相對於整個臺灣西南海域，是一個呈西北-東南走向相當狹窄的區域（約20公里寬），向外海加積的沈積物大多數越過陸棚區而直接輸送到高屏陸坡，然而，該陸坡受區域性構造擠壓抬升及泥貫入體活動的影響，形成數個陸坡盆地而成為主要接收臺灣造山帶沈積物的區域。高屏陸坡盆地的規模和形狀變化受控於泥貫入體抬升活動和沈積物的堆積，沈積物源分為由臺灣造山帶帶來向外海加積的遠端來源，以及因盆地邊緣邊坡不穩定崩塌的近端來源。高屏陸坡盆地震測相的垂直分佈群組(assemblage)多為聚合狀反射相、混亂反射相及平行簾狀反射相互相組合，平面分佈則以聚合狀反射相及混亂反射相廣泛分佈於水深2000公尺以上水域，平行簾狀反射相則僅發現於水深1000公尺以上的上部陸坡。高屏陸坡盆地內的堆積模式，先透過遠端造山帶的沈積物加積或偶發的濁流作用堆積在造山楔上（楔形體上方堆積區），然後經過同時的造山擠壓及泥貫入體抬升作用使沈積物產生向上傾斜(tilting)形成聚合狀沈積特徵，伴隨泥貫入體抬升作用持續進行，陸坡盆地邊緣產生邊坡不穩定的近端沈積物崩塌作用，形成無明顯層理的混亂相堆積，高屏海底峽谷西側淺於1000公尺的淺海區域，相對造山活動趨於穩定，沈積環境逐漸安定，沈積物則以平行散佈及懸浮沈降的方式堆積在陸坡盆地的最表層形成平行狀的震測相。
臺灣西南海域中，沈積物傳輸的另外一個重要方式是經由海底峽谷。高屏海底峽谷與澎湖海底峽谷為臺灣西南前陸盆地中最為明顯的兩條大型海底峽谷，與陸上河流直接相連的高屏海底峽谷承接大部分出自高屏溪的沈積物並將其輸往南海堆積，為典型的直接由鄰近造山帶橫向（transverse）傳送沈積物到前陸盆地中堆積的海底峽谷。澎湖海底峽谷位於碰撞軸部海床上，臺灣西南前陸盆地最前緣與穩定大陸邊緣相鄰的海底峽谷，峽谷流徑幾乎平行且遠離臺灣造山帶，而且不與陸上河流相接，為臺灣西南前陸盆地沈積物縱向（longitudinal）傳輸進入盆地內堆積最重要的管道，同時接受來自東側臺灣、西側中國東南邊緣以及北側臺灣海峽三個方向的沈積物並將其輸送到南中國海海盆。從形貌及內部沈積作用特徵，可將澎湖海底峽谷重新命名為澎湖海底峽谷-水道系統。澎湖海底峽谷-水道系統的發育與臺灣造山活動演化與西南前陸盆地前緣的遷移有關，整體流徑的發育演化主要受控於兩大因子，除了峽谷本身軸部順坡侵蝕下切外，承襲並襲奪（capture）源自南中國海陸坡上的峽谷-水道系統末端流徑，使其共同組成一個完整的水系，是形成整體流徑改變另外一個的重要的因素。目錄
摘要 Ⅰ
圖目錄 Ⅵ
表目錄 Ⅹ
第一章 序論 p.1
1-1 前陸盆地研究的必要性及定義 p.3
1-2 臺灣西部前陸盆地 p.5
1-3 臺灣西南前陸盆地 p.6
1-4 高屏陸坡盆地及澎湖海底峽谷 p.8
1-4-1 沈積物從來源到堆積地的過程 p.8
1-4-2 高屏陸坡盆地的構造及沈積特性 p.9
1-4-3 澎湖海底峽谷與前陸盆地的意義 p.10
1-4-4 高屏陸坡盆地及澎湖海底峽谷的文獻回顧 p.10
1-5 本文研究之目的及重要性 p.20
第二章 地質背景 p.22
2-1 臺灣區域地質及地球物理概述 p.22
2-1-1 臺灣島及周邊海域的地形地貌與地質分區 p.22
2-1-2 臺灣地區地球物理概述 p.26
2-1-3 臺灣周圍海域海床沈積物 p.31
2-1-4 臺灣周圍板塊活動與大地構造 p.32
2-1-5 臺灣造山機制及演化模式 p.34
2-2 臺灣西南陸域及海域的地質架構 p.44
2-2-1 地形地貌 p.44
2-2-2 臺灣西南區域的地層及沈積環境架構 p.47
2-2-3 臺灣西南區域的構造特徵 p.57
2-3 臺灣西南海域大地構造的論述及爭議 p.60
第三章 研究區域與方法 p.62
3-1 區域 p.62
3-2 方法與資料 p.63
3-2-1 方法 p.63
3-2-2 資料來源與規格 p.63
3-2-3 資料處理流程 p.63
3-2-4 資料應用方向 p.64
第四章 高屏陸坡盆地 p.66
4-1 震測相分類及可能的沈積作用 p.66
4-2 震測剖面描述 p.67
4-3 高屏上部陸坡沈積物厚度、陸坡盆地及震測相分佈 p.81
4-3-1 陸坡盆地及沈積物厚度分佈 p.81
4-3-2 陸坡盆地內震測相的分佈 p.82
4-4 討論 p.83
4-4-1 陸坡盆地的形成 p.83
4-4-2 形貌與沈積作用的關係 p.85
4-4-3 高屏陸坡盆地的堆積模式 p.87
4-4-4 小結 p.89
第五章 澎湖海底峽谷-水道系統 p.91
5-1 平面分佈 p.91
5-2 水深及震測剖面 p.92
5-2-1 水深剖面形貌的分類與可能的沈積作用 p.93
5-2-2 震測相的分類與可能的沈積作用 p.94
5-2-3 水深及震測剖面描述 p.95
5-2-4 小結 p.119
5-3 討論 p.121
5-3-1 形貌 p.121
5-3-2 形貌變化與谷道內沈積作用的關係 p.125
5-3-3 形貌變化與大地構造間的關係 p.129
5-3-4 海底峽谷襲奪及演化 p.130
5-3-5 小結 p.133
第六章 綜合討論 p.135
6-1 澎湖海底峽谷-水道系統與Markham海底峽谷比較 p.135
6-2 高屏陸坡盆地和墨西哥灣深水陸坡盆地比較 p.138
第七章 結論 p.141
參考文獻 p.14
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