File:NDL1017901 輓近の地震学 part2.pdf

From Wikimedia Commons, the free media repository
Jump to navigation Jump to search
Go to page
next page →
next page →
next page →

Original file(6,154 × 3,987 pixels, file size: 48.9 MB, MIME type: application/pdf, 82 pages)

Captions

Captions

Add a one-line explanation of what this file represents

Summary

[edit]
輓近の地震学   (Wikidata search (Cirrus search) Wikidata query (SPARQL)  Create new Wikidata item based on this file)
Author
松山, 基範, 1884-1958
image of artwork listed in title parameter on this page
Title
輓近の地震学
Publisher
大阪毎日新聞社[ほか]
Description

共同刊行: 東京日日新聞社 (東京)

附: 関東大地震の性質.但馬大地震の研究
Language jpn
Publication date

1925

大正14
Place of publication JP
Source

doi:10.11501/1017901

institution QS:P195,Q477675
Creator
InfoField
松山基範 著
Publication Place
InfoField
大阪
Subject: NDC
InfoField
453
Extent
InfoField
269, 64p ; 23cm
Material Type
InfoField
Book
Source Identifier: JPNO
InfoField
43050120
Date Digitized: W3CDTF
InfoField
2010-03-31
Audience
InfoField
一般
Title Transcription
InfoField
バンキン ノ ジシンガク
Publisher Transcription
InfoField
オオサカ マイニチ シンブンシャ
Source Identifier: NDLBibID
InfoField
000000597411
Call Number
InfoField
542-68
Creator Transcription: NDLNA
InfoField
マツヤマ, モトノリ
Creator: NDLNAId
InfoField
00042789
Contents
InfoField
第五節 走時線/182

第六節 初期微動繼續時間/185

第七節 震源の深さの影響/187

第八章 岩石の彈性波/190

第一節 地震波/190

第二節 彈性率とポアソン比/191

第三節 抗壓率/193

第四節 剛性率/195

第五節 彈性運動の式/197

第六節 變容波/199

第七節 縱波/201

第八節 非變容波/202

第九節 横波/204

第十節 岩石内の彈性波の速さ/205

第九章 地震の波動/207

第一節 地震波の速さ/207

第二節 初動の方向/209

第三節 主要動の性質/211

第四節 初動の引きと押しとの配置/214

第五節 天龍川地震の例/215

第六節 淡路島地震の例/217

第七節 彈性運動の他の解/218

第八節 陷落地震の變容波/220

第九節 陷落地震の非變容波/224

第十節 地辷り/227

第十一節 裂罅地震の變容波/227

第十二節 斷層/231

第十三節 裂罅地震の非變容波/232

第十四節 關東大地震に於ける初動の配置/236

第十五節 地質構造發達の一面/236

第十六節 津浪の初動/237

第十章 地球内部の構造の研究に於ける地震の貢献/241

第一節 震波の射出角/241

第二節 震波の經路/246

第三節 種々の深さでの震波の速さ/247

第四節 岩石圈と鐵核/252

第十一章 地震の原因/255

第一節 地球の冷却問題/255

第二節 ラヂウムの爲めに地球内に熱の發生/257

第三節 山脈は横壓力によつて出來たか/258

第四節 地殻の等壓的状態/260

第五節 調節運動/262

第六節 岩石の變形/264

第七節 大陸浮動説/266

附録 關東大地震の性質

一、 被害の分布/1

二、 震源地/7

三、 震波の傳播/14

四、 地殻の隆起及低下/17

五、 今回の地震の性質及原因/23

結論/37

但馬大地震の研究

一、 地震の體驗/39

二、 火災の慘害/43

三、 震災の分布/45

四、 地震計の記録/48

五、 破壞の始まり方/50

六、 震源の深さ/52

七、 地上の變動/54

八、 地震の強さ/58

九、 初動の方向/60

Licensing

[edit]
This image is in the public domain because it is a mere mechanical scan or photocopy of a public domain original, or – from the available evidence – is so similar to such a scan or photocopy that no copyright protection can be expected to arise. The original itself is in the public domain for the following reason:
Public domain
According to Japanese Copyright Law (June 1, 2018 grant) the copyright on this work has expired and is as such public domain. According to articles 51, 52, 53 and 57 of the copyright laws of Japan, under the jurisdiction of the Government of Japan works enter the public domain 50 years after the death of the creator (there being multiple creators, the creator who dies last) or 50 years after publication for anonymous or pseudonymous authors or for works whose copyright holder is an organization.

Note: The enforcement of the revised Copyright Act on December 30, 2018 extended the copyright term of works whose copyright was valid on that day to 70 years. Do not use this template for works of the copyright holders who died after 1967.

Use {{PD-Japan-oldphoto}} for photos published before December 31, 1956, and {{PD-Japan-film}} for films produced prior to 1953. Public domain works must be out of copyright in both the United States and in the source country of the work in order to be hosted on the Commons. The file must have an additional copyright tag indicating the copyright status in the United States. See also Copyright rules by territory.

العربية  Deutsch  English  español  français  Bahasa Indonesia  italiano  日本語  한국어  македонски  português  русский  українська  中文(简体)  中文(繁體)  +/−

You must also include a United States public domain tag to indicate why this work is in the public domain in the United States.

This tag is designed for use where there may be a need to assert that any enhancements (eg brightness, contrast, colour-matching, sharpening) are in themselves insufficiently creative to generate a new copyright. It can be used where it is unknown whether any enhancements have been made, as well as when the enhancements are clear but insufficient. For known raw unenhanced scans you can use an appropriate {{PD-old}} tag instead. For usage, see Commons:When to use the PD-scan tag.


Note: This tag applies to scans and photocopies only. For photographs of public domain originals taken from afar, {{PD-Art}} may be applicable. See Commons:When to use the PD-Art tag.

File history

Click on a date/time to view the file as it appeared at that time.

Date/TimeThumbnailDimensionsUserComment
current13:19, 7 November 2023Thumbnail for version as of 13:19, 7 November 20236,154 × 3,987, 82 pages (48.9 MB)Wmr-bot (talk | contribs)上載《1017901_2.pdf》

The following page uses this file:

Metadata