The Geology & Petrography of Timjaghas and its Environs
6 Angebote vergleichen
Bester Preis: Fr. 43.55 (€ 44.50)¹ (vom 02.05.2019)1
The Geology & Petrography of Timjaghas and its Environs
~EN PB NW
ISBN: 9783330001978 bzw. 3330001976, vermutlich in Englisch, LAP Lambert Academic Publishing, Taschenbuch, neu.
Lieferung aus: Deutschland, Versandkostenfrei.
The Geology & Petrography of Timjaghas and its Environs: The study area of Timjaghas lies between Latitude 09?19` 00 N to 09?20` 30 N and Longitude 09? 9` 00 E to 09? 13` 30 E on the Pankshin sheet 190NW. It is part of the Panyam Volcanic line. Geologically, the study area is characterized by the newer basalt and the biotite granite. The newer basalt is believed to be Tertiary in age. These basaltic rocks have been weathered forming laterites. The biotite granite is also underlain which is part of the Basement Complex was extruded by the volcanoes. Structurally, the study area has features such as veins, fractures and joints with structural trends in the NW-SE direction. Petrographically, the major minerals observed are plagioclase, olivine, amphibole, and quartz and accessory minerals such as zircon, opaque, iron oxide. Economically the rocks are not very important but can be useful in engineering geology in terms of construction materials. Englisch, Taschenbuch.
The Geology & Petrography of Timjaghas and its Environs: The study area of Timjaghas lies between Latitude 09?19` 00 N to 09?20` 30 N and Longitude 09? 9` 00 E to 09? 13` 30 E on the Pankshin sheet 190NW. It is part of the Panyam Volcanic line. Geologically, the study area is characterized by the newer basalt and the biotite granite. The newer basalt is believed to be Tertiary in age. These basaltic rocks have been weathered forming laterites. The biotite granite is also underlain which is part of the Basement Complex was extruded by the volcanoes. Structurally, the study area has features such as veins, fractures and joints with structural trends in the NW-SE direction. Petrographically, the major minerals observed are plagioclase, olivine, amphibole, and quartz and accessory minerals such as zircon, opaque, iron oxide. Economically the rocks are not very important but can be useful in engineering geology in terms of construction materials. Englisch, Taschenbuch.
2
Symbolbild
The Geology & Petrography of Timjaghas and its Environs (2019)
~EN PB NW
ISBN: 9783330001978 bzw. 3330001976, vermutlich in Englisch, LAP Lambert Academic Publishing Mrz 2019, Taschenbuch, neu.
Lieferung aus: Deutschland, Versandkostenfrei.
Von Händler/Antiquariat, AHA-BUCH GmbH [51283250], Einbeck, Germany.
Neuware - The study area of Timjaghas lies between Latitude 09°19' 00 N to 09°20' 30 N and Longitude 09° 9' 00 E to 09° 13' 30 E on the Pankshin sheet 190NW. It is part of the Panyam Volcanic line. Geologically, the study area is characterized by the newer basalt and the biotite granite. The newer basalt is believed to be Tertiary in age. These basaltic rocks have been weathered forming laterites. The biotite granite is also underlain which is part of the Basement Complex was extruded by the volcanoes. Structurally, the study area has features such as veins, fractures and joints with structural trends in the NW-SE direction. Petrographically, the major minerals observed are plagioclase, olivine, amphibole, and quartz and accessory minerals such as zircon, opaque, iron oxide. Economically the rocks are not very important but can be useful in engineering geology in terms of construction materials. 96 pp. Englisch.
Von Händler/Antiquariat, AHA-BUCH GmbH [51283250], Einbeck, Germany.
Neuware - The study area of Timjaghas lies between Latitude 09°19' 00 N to 09°20' 30 N and Longitude 09° 9' 00 E to 09° 13' 30 E on the Pankshin sheet 190NW. It is part of the Panyam Volcanic line. Geologically, the study area is characterized by the newer basalt and the biotite granite. The newer basalt is believed to be Tertiary in age. These basaltic rocks have been weathered forming laterites. The biotite granite is also underlain which is part of the Basement Complex was extruded by the volcanoes. Structurally, the study area has features such as veins, fractures and joints with structural trends in the NW-SE direction. Petrographically, the major minerals observed are plagioclase, olivine, amphibole, and quartz and accessory minerals such as zircon, opaque, iron oxide. Economically the rocks are not very important but can be useful in engineering geology in terms of construction materials. 96 pp. Englisch.
3
The Geology & Petrography of Timjaghas and its Environs
~EN NW
ISBN: 9783330001978 bzw. 3330001976, vermutlich in Englisch, neu.
Lieferung aus: Vereinigtes Königreich Grossbritannien und Nordirland, Lieferzeit: 11 Tage, zzgl. Versandkosten.
The study area of Timjaghas lies between Latitude 09°19' 00 N to 09°20' 30 N and Longitude 09° 9' 00 E to 09° 13' 30 E on the Pankshin sheet 190NW. It is part of the Panyam Volcanic line. Geologically, the study area is characterized by the newer basalt and the biotite granite. The newer basalt is believed to be Tertiary in age. These basaltic rocks have been weathered forming laterites. The biotite granite is also underlain which is part of the Basement Complex was extruded by the volcanoes. Structurally, the study area has features such as veins, fractures and joints with structural trends in the NW-SE direction. Petrographically, the major minerals observed are plagioclase, olivine, amphibole, and quartz and accessory minerals such as zircon, opaque, iron oxide. Economically the rocks are not very important but can be useful in engineering geology in terms of construction materials.
The study area of Timjaghas lies between Latitude 09°19' 00 N to 09°20' 30 N and Longitude 09° 9' 00 E to 09° 13' 30 E on the Pankshin sheet 190NW. It is part of the Panyam Volcanic line. Geologically, the study area is characterized by the newer basalt and the biotite granite. The newer basalt is believed to be Tertiary in age. These basaltic rocks have been weathered forming laterites. The biotite granite is also underlain which is part of the Basement Complex was extruded by the volcanoes. Structurally, the study area has features such as veins, fractures and joints with structural trends in the NW-SE direction. Petrographically, the major minerals observed are plagioclase, olivine, amphibole, and quartz and accessory minerals such as zircon, opaque, iron oxide. Economically the rocks are not very important but can be useful in engineering geology in terms of construction materials.
4
The Geology & Petrography of Timjaghas and its Environs (2019)
~EN PB NW
ISBN: 9783330001978 bzw. 3330001976, vermutlich in Englisch, 96 Seiten, LAP Lambert Academic Publishing, Taschenbuch, neu.
Lieferung aus: Deutschland, Versandkosten nach: Deutschland, Versandkostenfrei.
Von Händler/Antiquariat, Syndikat Buchdienst, [4235284].
The study area of Timjaghas lies between Latitude 0919' 00 N to 0920' 30 N and Longitude 09 9' 00 E to 09 13' 30 E on the Pankshin sheet 190NW. It is part of the Panyam Volcanic line. Geologically, the study area is characterized by the newer basalt and the biotite granite. The newer basalt is believed to be Tertiary in age. These basaltic rocks have been weathered forming laterites. The biotite granite is also underlain which is part of the Basement Complex was extruded by the volcanoes. Structurally, the study area has features such as veins, fractures and joints with structural trends in the NW-SE direction. Petrographically, the major minerals observed are plagioclase, olivine, amphibole, and quartz and accessory minerals such as zircon, opaque, iron oxide. Economically the rocks are not very important but can be useful in engineering geology in terms of construction materials. 2019, Taschenbuch / Paperback, Neuware, H: 220mm, B: 150mm, 96, Internationaler Versand, Selbstabholung und Barzahlung, PayPal, offene Rechnung, Banküberweisung.
Von Händler/Antiquariat, Syndikat Buchdienst, [4235284].
The study area of Timjaghas lies between Latitude 0919' 00 N to 0920' 30 N and Longitude 09 9' 00 E to 09 13' 30 E on the Pankshin sheet 190NW. It is part of the Panyam Volcanic line. Geologically, the study area is characterized by the newer basalt and the biotite granite. The newer basalt is believed to be Tertiary in age. These basaltic rocks have been weathered forming laterites. The biotite granite is also underlain which is part of the Basement Complex was extruded by the volcanoes. Structurally, the study area has features such as veins, fractures and joints with structural trends in the NW-SE direction. Petrographically, the major minerals observed are plagioclase, olivine, amphibole, and quartz and accessory minerals such as zircon, opaque, iron oxide. Economically the rocks are not very important but can be useful in engineering geology in terms of construction materials. 2019, Taschenbuch / Paperback, Neuware, H: 220mm, B: 150mm, 96, Internationaler Versand, Selbstabholung und Barzahlung, PayPal, offene Rechnung, Banküberweisung.
5
Symbolbild
The Geology & Petrography of Timjaghas and its Environs
~EN PB NW
ISBN: 9783330001978 bzw. 3330001976, vermutlich in Englisch, Taschenbuch, neu.
Lieferung aus: Deutschland, Versandkostenfrei.
Von Händler/Antiquariat, European-Media-Service Mannheim [1048135], Mannheim, Germany.
Die Beschreibung dieses Angebotes ist von geringer Qualität oder in einer Fremdsprache. Trotzdem anzeigen
Von Händler/Antiquariat, European-Media-Service Mannheim [1048135], Mannheim, Germany.
Die Beschreibung dieses Angebotes ist von geringer Qualität oder in einer Fremdsprache. Trotzdem anzeigen
6
Symbolbild
The Geology & Petrography of Timjaghas and its Environs (2019)
EN PB NW
ISBN: 9783330001978 bzw. 3330001976, in Englisch, 96 Seiten, LAP Lambert Academic Publishing, Taschenbuch, neu.
Lieferung aus: Deutschland, Gewöhnlich versandfertig in 24 Stunden, Versandkostenfrei. Tatsächliche Versandkosten können abweichen.
Von Händler/Antiquariat, averdo24.
Die Beschreibung dieses Angebotes ist von geringer Qualität oder in einer Fremdsprache. Trotzdem anzeigen
Von Händler/Antiquariat, averdo24.
Die Beschreibung dieses Angebotes ist von geringer Qualität oder in einer Fremdsprache. Trotzdem anzeigen
Lade…