登录注册
Quick Links : Mindat手册The Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
主页关于 MindatMindat手册Mindat的历史版权Who We Are联系我们于 Mindat.org刊登广告
捐赠给 MindatCorporate Sponsorship赞助板页已赞助的板页在 Mindat刊登 广告的广告商于 Mindat.org刊登广告
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
搜索矿物的性质搜索矿物的化学Advanced Locality Search随意显示任何一 种矿物Random Locality使用minID搜索邻近产地Search Articles搜索词汇表更多搜索选项
搜索:
矿物名称:
地区产地名称:
关键字:
 
Mindat手册添加新照片Rate Photos产区编辑报告Coordinate Completion Report添加词汇表项目
Mining Companies统计会员列表Mineral MuseumsClubs & Organizations矿物展及活动The Mindat目录表设备设置The Mineral Quiz
照片搜索Photo GalleriesSearch by Color今天最新的照片昨天最新的照片用户照片相集过去每日精选照片相集Photography

(1916) I.—The Petrography of Arran. Geological Magazine, S. 6 Vol. 3 (5) 193-196 doi:10.1017/s0016756800199789

Advanced
   -   Only viewable:
Reference TypeJournal (article/letter/editorial)
TitleI.—The Petrography of Arran
JournalGeological Magazine
Year1916 (May)Series:Volume6:3
Page(s)193-196Issue5
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800199789
Mindat Ref. ID264679Long-form Identifiermindat:1:5:264679:8
GUID523cc959-c1b4-4a92-9034-a76b2c068507
Full Reference(1916) I.—The Petrography of Arran. Geological Magazine, S. 6 Vol. 3 (5) 193-196 doi:10.1017/s0016756800199789
Plain Text(1916) I.—The Petrography of Arran. Geological Magazine, S. 6 Vol. 3 (5) 193-196 doi:10.1017/s0016756800199789
In(1916, May) Geological Magazine S. 6 Vol. 3 (5) Cambridge University Press (CUP)
Abstract/NotesThe phenomenon of which this paper treats occurs in a basalt dyke exposed in a small quarry by the roadside north-east of Dippin, near the twelfth milestone from Brodick. This dyke runs from north-west to south-east, and is intrusive into the great teschenite (or crinanite) sill of Dippin. It is probably the one referred to in the Geological Survey Memoir on North Arran, South Bute, and the Cumbraes (1903), p. 119. It averages 12 feet in thickness, although it is extremely irregular, owing perhaps to the difficulty experienced in penetrating the tough, coarse, massive rock of the sill. The contacts are not plane, but about against the crinanite in a very intricate manner, sometimes along vertical or horizontal joints, sometimes along irregular surfaces unconnected with jointing. Both contacts show thin films of tachylyte, which, as the rock is quarried, are left adhering to the irregular surfaces of the sill rock. Another dyke-like mass, 1 foot thick, is seen in the same quarry, and is doubtless an offshoot from the larger dyke.

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

Igneous Rocks and their Origin, 1914, p. 212.
Scott (1914) Trans. Geol. Soc. Pitchstones of South Arran xv, 22
Clarke (1911) Data of Geochemistry , 279
Iddings (1909) Igneous Rocks i, 85
Lacroix (1893) Les Enclaves des Roches Volcaniques , 563


See Also

These are possibly similar items as determined by title/reference text matching only.

 
矿物 and/or 产地  
Mindat Discussions Facebook Logo Instagram Logo Discord Logo
版权所有© mindat.org1993年至2024年,除了规定的地方。 Mindat.org全赖于全球数千个以上成员和支持者们的参与。
隐私政策 - 条款和条款细则 - 联络我们 - Report a bug/vulnerability Current server date and time: 2024.5.2 10:03:31
Go to top of page