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Write a review Rate this item: Please verify that you are not a robot. Local factors influencing in-situ stress have been identified in these zones of the tunnels, related to geological structures of high compressive tectonic stress regimes including thrust faults, folds with steep flank dip, or with geomechanical anisotropies in contact zones between rock formations of different ingenidria.

Spanish View all editions and formats. Your request to send this item has been completed. Create lists, bibliographies and reviews: You already recently rated this item. Reply to comment from Blanco et al.

The case of Pajares tunnels, Spain more. Bulletin of Engineering Geology and the Environment. The E-mail Address es field is required. This significant increase in gwologica magnitude of in-situ stress emphasises the influence of geological ognzalez geomechanical anisotropies in tunnel stability and support design. Engineering geology of the tropical volcanic soils of La Laguna, Tenerife more.

SRC rock mass classification of tunnels under high tectonic stress excavated in weak rocks more. The E-mail message field is required.


Ingeniería geológica

Civil Engineering and Engineering Geology. Kregional was estimated from hydrofracture tests and from the TSI index. Please re-enter recipient e-mail address es.

Four tunnels for the new high-speed railway lines in Pajares in the Cantabrian Mountains, N. The specific requirements or preferences of your vllejo publisher, classroom teacher, institution or organization should be applied.

Ingeniería geológica (Book, ) []

Add a review and share your thoughts with other readers. Home About Help Search. Citations are based on reference standards. A methodological procedure was applied to four tunnels to assess the influence of the geological anisotropies on the in-situ stress magnitudes. Four tunnels for the new high-speed railway lines in Pajares in the Cantabrian Find a copy in the library Finding libraries that hold this item Une procedure generale pour la cartographie regionale sismotectonique en vue de son utilisation en genie civil more.

Your rating has been recorded. The soil fabric is considered to be the main factor leading to these unusual properties, but geochemical environment and associated mineralogy also play an important part. ABSTRACT Geological and geomechanical anisotropies can significantly increase the magnitude of in-situ stress in a rock mass excavated for tunnelling purposes.

Ingenieria Geologica by Gonzalez De Vallejo Luis I – Hardcover

Journal of Volcanology and Geothermal Research. Emphasis has been placed on the influence of mineralogy and fabric on the strength and deformation properties, and Spanish View all editions and formats Rating: Klocal was calculated from the back analysis of the support pressure required to stabilise the deformed tunnel zones.


Conspicuous sediment structures in fossil beach deposits southern Tenerife, Canary Islands, Spain: Please enter the message. Emphasis has been placed on the influence of ingenieris and geologixa on the strength and deformation properties, and particularly on the results of gellogica classification test.

The E-mail Address es you entered is are not in a valid format. Civil EngineeringGeophysicsand Canary Islands. The name field is required. Please choose whether or not you want other users to be able to see on your profile that this library is a favorite of yours.

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Ingenieria Geologica by Gonzalez De Vallejo Luis I – Hardcover | eBay

Engineering Geology an International Journal. Lecture Notes geloogica Earth Sciences. This procedure is based on the analysis of tunnel deformations and the support pressure needed to stabilise the excavations affected by geological anisotropies.

Click here to sign up. Engineering geology for urban planning and development with an example from tenerife Canary Islands more. You may have already requested this item. A new method of estimating the ratio between in situ rock stresses and tectonics based on empirical and probabilistic analyses more. Remember me on this computer. Your Web geollogica is not enabled for JavaScript.

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