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Search Symbol (Half-width) Description of Search Symbols
Space "AND" indicates the intertwining of key terms used in a search
Double Quotation Marks ("") ( " " ) Double quotation marks indicate the beginning and end of a phrase, and the search will only include terms that appear in the same order of those within the quotations. Example: "image process" : " image process "
? Indicates a variable letter. Entering two ? will indicate two variable letters, and so on. Example: "Appl?", search results will yield apple, apply… e , appl y … ( (often used to English word searches) )
* Indicates an unlimited number of variable letters to follow, from 1~n. Example: Enter "appl*", search results will yield apple, apples, apply, applied, application…(often used in English word searches) e , appl es , appl y , appl ied , appl ication … ( (often used to English word searches) )
AND、OR、NOT

Boolean logic combinations of key words is a skill used to expand or refine search parameters.
(1) AND (1) AND: Refines search parameters
(2) OR (2) OR: Expands search parameters (3) NOT: Excludes irrelevant parameters

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DOI stands for Digital Object Identifier ( D igital O bject I dentifier ) ,
and is the unique identifier for objects on the internet. It can be used to create persistent link and to cite articles.

Using DOI as a persistent link

To create a persistent link, add「http://dx.doi.org/」 「 http://dx.doi.org/ 」 before a DOI.
For instance, if the DOI of an article is 10.5297/ser.1201.002 , you can link persistently to the article by entering the following link in your browser: http://dx.doi.org/ 10.5297/ser.1201.002
The DOI link will always direct you to the most updated article page no matter how the publisher changes the document's position, avoiding errors when engaging in important research.

Cite a document with DOI

When citing references, you should also cite the DOI if the article has one. If your citation guideline does not include DOIs, you may cite the DOI link.

DOIs allow accurate citations, improve academic contents connections, and allow users to gain better experience across different platforms. Currently, there are more than 70 million DOIs registered for academic contents. If you want to understand more about DOI, please visit airiti DOI Registrationdoi.airiti.com ) 。

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Times Cited : (2)

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What is "Preprint"?

In order to provide readers the forefront academic information, after articles are accepted to publish in the journal, we publish them in network before they're printed. Those "on-line first articles" are called the "preprint articles". The preprint articles do not have volume No., page No., publication date, but can be identified by the DOI number. 「 http://dx.doi.org/ 」 Link to the latest version of the article.

How to cite Preprint Articles?

Please use the online publication date and the DOI number of the preprint article to cite the literature.

Cited example (may vary with different formats you cited):

Author name. Article name. Journal name. YYYY/MM/DD online publish in advance.

doi:DOI Number

Basic Information
Publisher

National Taiwan University

Taiwan

國立臺灣大學 Publishing 』

台大_NTU
2008年
Total5Pages
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21

南台灣恆春區域新期構造運動之研究

李珀儂

恆春半島恆春斷層西恆春斷層西恆春背斜西恆春台地上衝構造Hengchun FaultHengchun PeninsulaWestern Hengchun TablelandWestern Hengchun FaultWestern Hengchun AntiformPop-up structure

10.6342/NTU.2008.00190 DOI

Abstract | Reference(72) | Times Cited(6) Download Download PDF Add to Cart Add to Cart Track Track

22

利用微構造分析太麻里地區的變形歷史

徐乙君

壓影纖維構造變形歷史壓扁效應造成的葉理隱沒-碰撞的過渡帶太麻里pressure shadowsstrain historyflat-lying foliationsubduction-collision conjunctionTaimali

10.6342/NTU.2008.01341 DOI

Abstract | Reference(80) Download Download PDF Add to Cart Add to Cart Track Track

23

浮游有孔蟲Globigerinoides fistulosus消失 與熱帶太平洋表水水文變化關係

陳貞吟

Globigerinoides fistulosusG. sacculifer西太平洋暖池氧碳同位素鎂鈣元素比雷諾數更新世—上新世邊界Globigerinoides fistulosusG. sacculiferWestern Pacific Warm Pooloxygen and carbon isotopeMg/Ca ratiosReynolds NumberPliocene/Pleistocene boundary

10.6342/NTU.2008.00336 DOI

Abstract | Reference(20) | Times Cited(2) Download Download PDF Add to Cart Add to Cart Track Track

24

西赤道太平洋所羅門海ODP1115B站位上部上新統至更新統鈣質超微化石生物地層硏究

莊智凱

西太平洋暖池ODP1115B第四紀鈣質超微化石生物地層western pacific warm pool, ODP1115B, Quaternary, calcareous nannofossil, biostratigraphy

10.6342/NTU.2008.00652 DOI

Abstract | Reference(69) | Times Cited(2) Download Download PDF Add to Cart Add to Cart Track Track

25

嘉義地區的相對構造活動速率及其與地表地形的相關性:利用河流水力侵蝕模型

黃筱婷

嘉義地區構造活動地形學地形計測指標河流水力侵蝕模型河流凹曲度河流陡峭程度指標Chiayi AreaTectonic ActivitiesGeomorphologyGeomorphic IndexesStream Power Incision ModelRiver Concavity (m/n ratio)Normalized Steepness Index (ksn)

10.6342/NTU.2008.01599 DOI

Abstract | Reference(90) | Times Cited(2) Download Download PDF Add to Cart Add to Cart Track Track

26

中子井測應用於分析岩體裂隙及孔隙率之研究

曾何騰

中子井測裂隙孔隙率中子孔隙率指標neutron logfractureporosityneutron porosity index

10.6342/NTU.2008.00063 DOI

Abstract | Reference(34) | Times Cited(1) Download Download PDF Add to Cart Add to Cart Track Track

27

利用永久散射體雷達干涉技術分析地表變形:以臺灣西南部平原為例

童忻

差分合成孔徑雷達干涉技術永久散射體雷達干涉技術台南台地後甲里斷層大灣低地雲林縣地表變形地層下陷InSARDInSARPSInSARTainan TablelandHouchiali FaultTawan LowlandYunlin CountySurface DeformationLand Subsidence

10.6342/NTU.2008.01604 DOI

Abstract | Reference(71) | Times Cited(6) Download Download PDF Add to Cart Add to Cart Track Track

28

華南南嶺地區早燕山期(侏羅紀)侵入岩定年學、全岩地球化學、鍶-釹同位素與磷灰石地球化學研究與地體構造意義

謝佩珊

中生代花崗岩鋯石鈾-鉛定年磷灰石地球化學南嶺華南Mesozoic granitoidsNanling MountainsSouth China

10.6342/NTU.2008.03091 DOI

Abstract | Reference(177) Download Download PDF Add to Cart Add to Cart Track Track

29

台灣新第三系有機物熱成熟指標之探討

沈俊卿

有機物成熟度生物指標天然氣生成沉積環境CoalShaleBiomarkerVitriniteOrganic MaturitySedimentary environment

10.6342/NTU.2008.02707 DOI

Abstract | Reference(153) | Times Cited(1) Download Download PDF Add to Cart Add to Cart Track Track

30

緬甸晚新生代火山岩之地球化學及岩石成因

楊曉明

緬甸晚新生代火山岩高鉀鈣鹼系列Sagaing斷層小程度部分熔融氬氬定年MyanmarBurmaHigh-K calc-alkaline suiteSagaing faultsmall-degree partial meltingAr-Ar dating

10.6342/NTU.2008.02870 DOI

Abstract | Reference(48) | Times Cited(1) Download Download PDF Add to Cart Add to Cart Track Track

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Total 5 Pages
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