Asymptotics for Maxwell-Chern-Simons multivortices by Ricciardi T.

By Ricciardi T.

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7, 16 in Chapter 9). Difficulties in interpretation of log patterns may result from deviations of individual facies successions from the general model in Figure 7, possibly in 1 Cylindrical Funnel Shaped Bell Shaped Symmetrical Clean, No Trend Abrupt Top Coarsening Upward Abrupt Base Fining Upward Rounded Base and Top 0 150 aeolian, braided fluvial, carbonate shelf, reef, submarine canyon fill 0 \ . ~ 150 crevasse splay, distributary mouth bar, ciastic strand plain, barrier island. shallow marine sheet sandstone, carbonate shoalingupward sequence.

Some newly developed methods in subsurface sedimentology, such as the use of resistivity microscanners to detect sedimentary structures, and the analysis of high-resolution dipmeter data, are as yet not widely applied, but are discussed by Hurst et a/. (1990). The two major types of data, subsurface geological and geophysical, will be treated separately, but where available, both can be integrated. CANT 10-13-63-21w 4 Resistivity (ohms~m2/m) 0 GEOLOGICAL USES OF WELL LOGS Well logs are made by pulling an instrumented tool up the hole, and recording the data as a function of depth.

It must be emphasized that the gamma-ray reading is not a function of grain size or carbonate content, only of the proportion of radioactive elements, which may be related to the proportion of shale. For example&yfree sandstones or conglomerates with any mix of sand and pebble clast sizes generally give similar responses, and lime mudstone gives the same response as grainstone. Distinguishing between clean (clay-free) lithologies such as sandstones, conglomerates, dolomites, and limestones is best done by calibration of one or more logs to cores or cuttings.

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