isocline


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i·so·cline

 (ī′sə-klīn′)
n. Geology
An anticline or syncline so tightly folded that the rock beds of the two sides are nearly parallel.

isocline

(ˈaɪsəʊˌklaɪn)
n
1. (Geological Science) a series of rock strata with isoclinal folds
2. (Geological Science) another name for isoclinal3
Translations
jafnhallaferill
References in periodicals archive ?
to construct the outlines of the morphologic elements in parallel plans and to define the isocline curves.
q] = 0 isocline is always defined at m'(k*) = [rho] + [omega] + [theta].
The steady state of (P) is a local saddlepoint if and only if the slope of the [Mathematical Expression Omitted] isocline is greater than the slope of the [Mathematical Expression Omitted] isocline, evaluated at the steady state.