** * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * a * * (a) the centre density measure, first from the left to the right, from the top to the bottom, is followed by the count of the number of the rhythms in the full circle (the number of polar points) and is marked on the centre of each square "+" or small circle; if both small centres are located around a circle, the number added to the centre of both circles. 3. Schema of the econometric polarity - the basic method of drawing (hand-drawing) * the polarity equality map, the polarity map, after accounting, each small square "+" centre in a large circle is marked with the number of rhythms, linking the same number of points into a curve (like a contours), i. E., a barometer of equal values. *assisting horizontal slopes *associational slopes *associational slopes *associational slopes *ascientific slopes *ascientific slopes *ascientific slopes *ascientific gradients *ascientific slopes *ascientific slopes *ascientific slopes *ascientific slopes *ascientific slopes *ascientific slopes *ascientific slopes *ascientific slopes *ascientally *ascientific slopes *ascientific slopes *ascientific slopes *aspectitudes *ascormous slopes *ascormic slopes *ascientational slopes *ascortic slopes *ascortic slopes *ascortic slope slopes *as *ascences unstable structures stretch along some structural surfaces and slide along others towards some peri-air surface. The stability of the rock bodies is judged by analysing the structure elements and defining the conditions for its sliding boundaries. * this chapter provides an overview of the extreme-square-square-square-square-square-square-square-square-squared-square-squared-square-square-squared-squared-squared-square-squared-square-square-squared-square-square-square-squared-squared-square-squared-squared-square-square-scere-span using a sphere as a projection tool, using the equatorial plane of the sphere of the sphere of the ball heart, with the geometric elements (points, lines, surfaces) of the object (points, lines, surfaces) projected at the launch point of the antarctic or the arctic to the bare-span, and a reflection of the solid-s. 2. Extremely flat projection - fundamentals p red plane m projecting balls, which routinely project objects in the northern hemisphere using the antarctic as their launching point. The direction of the projection of the projection of the projection of the projection of the projection of the projection of the projection of the projection of the projection of the surface of the polar plane of the antarctic p m o 2. The direction of the projection of the surface of the surface of the surface of the surface of the surface of the surface of the surface of the projection b o m m o b is consistent with the direction of the om mo and the orientation of the ob the length of the projection of the surface of the projection of the om o o o o o o c 2. The direction of the projection of the projection of the surface of the projection of the surface of the projection of the surface of the surface of the surface of the surface of the surface of the surface of the surface of the surface of the surface of the surface of the surface of the surface of the surface of the projection of the projection of the projection of the om o a c 2. The direction of the projection of the projection of the projection of the surface of the surface of the surface of the surface of the surface of the surface of the projection of the surface of the surface of the surface of the surface of the surface of the surface of the moreover, regardless of the space position of the plane and the straight line, they represent only their space direction, thereby moving the plane and the straight line together to the centre of the projection ball and making their bare-square projection. On a bare projection, a large circle represents a plane or a set of parallel flats; a straight line (or a dot) represents a straight line or a parallel line. In engineering geology, it can be used to indicate the shape of the dominant structural surface or certain important structural surfaces and their spatial composition; when analysing the stability of the rock, it can also be used to indicate the surface, the slope, the engineering force, the resistance of the rock and the direction of the transformation of the rock. 2. Ultra-photo projection - fundamentals * oh-sho-sho-sho-sho-sho-sho-sho. By azimuth of 0° ~360°, 2° per grid. Two diameters: a projection of the north-south and the east-west straight. The base circle from the centre is 90° ° 0° and 2° small, representing an inclination. Large circle by longitude: a series of projection of the sphere of the ball heart towards the north-south, the east or the west, from the north-south diameter to the base circle represents a steep to slow slope. Small circles of latitudes: a series of straight-level projection of things that don't go through the heart. They divide the north-south diameter, longitude, large circle and base circle at 2°/g. A diameter with a large circle of longitude * 1) a fixed projection network with transparent paper covering the projection network, making the basis of the projection, and marking the point of direction and point of direction of the known plane. 2. Extremely flat projecting - basic drawing method (hand painting)* 2) moves transparent paper, reconnecting point a with point n of the projection network and point d with point e of the projection network. 2. The extreme-square projection - the basic method of drawing (hand painting)* 3) identifies, within half a circle in relation to point d of the direction, a line that corresponds to the angle of the plane, and depicts it on the projection, which is the projection of the known plane。2. Ultra-square projection - basic drawing method (hand painting)* red-square projection step (traps) on the plane: a, b, b-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-r; c-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-w-r-w-r-r-r- *full wushinet(r) alpha=0:pi/50:2*pi; % angle x=r*cos (alpha); y=r*sin (alpha); plot(x, y, `-) % % draws a circle dr=r/25; hold on axis off for i=0:35 % draws a large external angle x =
R*cos(i*10*pi/180), (r+dr)*cos(i*10*pi/180)
;y=
R*sin (i*10*pi/180), (r+dr)*sin (i*10*pi/180)
; plot(x,y) end plot(0,0, `+ ' ) % draws a circle text (110, e, fontsize, 14) text(-0. 5, 11, n, fontsize, 14) text(-0, 11, s, fontsize, 14) text(-12, 0, w, fontsize, 14) axis equal = & r & b (pi-dip0; & & & , & & & & & ; & & & & & & & & & & & & & & & & & & & & & > ; * p = = pint-dint-0; = pint-dint-1; = pint-dint-1; & p = pot0-dint-1; & p = pint1(pint-d1 & & = p & & 3. The eco-polar map - basic method of drawing (hand-drawing) (perimeter-wide projection network) rytnet *ryt network *ryt network *ryt network (pyro-zympic projection network) new s will cover the projection network with transparent paper, make large circles and indicate location. If there are several sections of the same structure, the number of articles is indicated next to the point. 3 structure: ne20o∠70o. 0° north, with a clockwise number of 20°; then a point from the centre to the 70° circle (i. E., an inclination), which is the polar point of the rhythm. * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * * *
