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Petrophysical Properties of Crystalline Rocks (Geological by P. K. Harvey, T. S. Brewer, P. A. Pezard, V. A. Petrov

24 February 2017 adminNonfiction 3

By P. K. Harvey, T. S. Brewer, P. A. Pezard, V. A. Petrov

Boreholes are normally drilled into crystalline rocks to guage their suitability for numerous purposes corresponding to waste disposal (including nuclear waste), geothermal strength, hydrology, sequestration of greenhouse gases and for fault research. Crystalline rocks contain igneous, metamorphic or even a few sedimentary rocks. The quantification and figuring out of person rock lots calls for vast modelling and an research of varied actual and chemical parameters. This quantity covers the subsequent elements of the petrophysical houses of crystalline rocks: fracturing and deformation, oceanic basement reports, permeability and hydrology and laboratory-based reports. With the turning out to be calls for for sustainable and environmentally potent improvement of the subsurface, the petrophysics of crystalline rocks is changing into an more and more very important field.Also on hand: functions of X-ray Computed Tomography within the Geosciences - ISBN 1862391394 Hydrocarbons in Crystalline Rocks - ISBN 1862391378 Fracture And In-situ pressure Characterisation of Hydrocarbon Reservoirs - ISBN 1862391300

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Extra resources for Petrophysical Properties of Crystalline Rocks (Geological Society Special Publication No. 240)

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7). g. Pezard 1990). Therefore, the separation between the two logs indicates that vertical fracturing occurs throughout the sill, but decreases near the bottom where the two logs come together. In the sediments, the LLD and LLS resistivity logs overlie each other and measure much lower resistivity values. In general, deep-reading resistivity logs, like the LLD, more accurately represent undamaged formation properties and are used for porosity and lithology interpretation. Fractures filled with water are usually more conductive than the surrounding rock.

GIESE E T AL. 0 ......................... 0 : : =:~ :'~ . . 0 . 0 ......... . 5 . ,. 5 ~r . I . ->~ ............... 0 . ~- ::::~'~"~ " ,,,,~. 5 ~-~.............. 0 800 700 (Tm) Fig. 9. Seismic velocities Vp and Vs derived from tomographic inversions at 3 m distance from the tunnel wall of the Faido adit (dotted line). The solid lines through the velocity values are polynomial fitting curves. The cataclastic zones at Tm 973 and Tm 2410 are surrounded by wider zones with lower wave velocities, which mark the disturbance zones in the Leventina gneiss (cf.

3). Natural gamma logs record the total gamma radiation detected in a borehole, and they are the most widely used nuclear logs for stratigraphic investigations. Sediments are much more radioactive than basalt or other intrusive mafic rocks, and therefore a large increase in gamma-ray activity is observed at the dolerite-sediment contact. Caliper logs measure the diameter of the hole. The two wells appear to be generally smooth, without any large washout zones. 5 cm. A neutron porosity log in Well 2 is shown in Figure 7.

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