From 4b7d5e1d3201033c5788b555310038a3b9dbfc55 Mon Sep 17 00:00:00 2001 From: Rowan Cockett Date: Wed, 12 Mar 2014 23:08:58 -0700 Subject: [PATCH] Update api_PF.rst Get rid of conflict --- docs/api_PF.rst | 9 --------- 1 file changed, 9 deletions(-) diff --git a/docs/api_PF.rst b/docs/api_PF.rst index dc57d994..2fc0da1a 100644 --- a/docs/api_PF.rst +++ b/docs/api_PF.rst @@ -99,16 +99,7 @@ Since most materials in the earth have lower permeability than \\(\\mu_0\\), us Since we compute secondary field based on the earth field, which can be different from different locations in the world, we can expect different anomalous responses in different locations in the earth. For instance, assume we have two susceptible spheres, which are exactly same. However, anomalous responses in Seoul and Vancouver are going to be different. - -<<<<<<< Updated upstream .. plot :: examples/Mag_back_1.py -======= -.. plot :: - :include-source: - - from simpegPF.MagAnalytics import MagSphereAnalFunA - from SimPEG import * ->>>>>>> Stashed changes Since we can measure total fields ( \\(\\vec{B}\\)), and usually have reasonably accurate earth field (\\(\\vec{B}_0\\)), we can compute anmalous fields, \\(\\vec{B}_s\\) from our observed data. If you want to download earth magnetic fields at specific location see this website (`noaa `_).