dc.creator |
Aparicio, Alfredo |
|
dc.creator |
Bustillo, Mª Ángeles |
|
dc.creator |
García García, Roberto |
|
dc.creator |
Araña, Vicente |
|
dc.date |
2008-02-08T08:11:11Z |
|
dc.date |
2008-02-08T08:11:11Z |
|
dc.date |
2006 |
|
dc.date.accessioned |
2017-01-31T00:59:47Z |
|
dc.date.available |
2017-01-31T00:59:47Z |
|
dc.identifier |
Geological Magazine vol 143 paginas 181-193 |
|
dc.identifier |
http://hdl.handle.net/10261/2892 |
|
dc.identifier |
10.1017/S0016756806001713 |
|
dc.identifier.uri |
http://dspace.mediu.edu.my:8181/xmlui/handle/10261/2892 |
|
dc.description |
The xenoliths of dunites and other ultramafic rocks (peridotites ,wherlites..etc) are generated by contact metamorphism from sedimentary rocks |
|
dc.description |
proyecto FEDER "Aspectos educativos del volcanismo canario
Ministerio Educación Y Ciencia proyecto BTE2002-04017-Co2-1 |
|
dc.description |
Peer reviewed |
|
dc.format |
1106 bytes |
|
dc.format |
text/html |
|
dc.language |
eng |
|
dc.publisher |
Cambridge University Press |
|
dc.rights |
openAccess |
|
dc.subject |
metasedimentary xenoliths |
|
dc.subject |
dunites |
|
dc.title |
Metasedimentary xenoliths in the lavas of the Timanfaya eruption(1730-1736. Lanzarote, Canary Islands):metamorphism and contamination processes |
|
dc.type |
Artículo |
|