Presentation is loading. Please wait.

Presentation is loading. Please wait.

Attitude of Beds Attitude: A general term for the orientation of a line or plane. Attitude refers to the three dimensional orientation of planar and linear.

Similar presentations


Presentation on theme: "Attitude of Beds Attitude: A general term for the orientation of a line or plane. Attitude refers to the three dimensional orientation of planar and linear."— Presentation transcript:

1 Attitude of Beds Attitude: A general term for the orientation of a line or plane. Attitude refers to the three dimensional orientation of planar and linear features such as a bed, a joint, a hornblende neddle or a fold. The attitude of planar features, such as beds or joints, is defined by their strike and dip.

2 Attitude of Linear Structures
Attitude of Beds Attitude of Linear Structures The attitude of linear structures is defined by the trend & plunge (together they define a vector) Trend is the bearing of the line & Plunge is the inclination of the line. Linear structure are also defined by their pitch / rake on a given plane: Pitch / Rake: The acute angle between the line and the strike of the plane on which the line lies. Example of linear structures: Fold axis, hingeline, intersection of two planes, stretched pebbles, slickenside, other lineations. Plunge Horizontal line Line – linear structure Vertical Plane Inclined Plane Line – linear structure Horizontal line Pitch / Rake Inclined Plane

3 Attitude of Planar Structures
Attitude of Beds Attitude of Planar Structures The attitude of planar structures is defined by the strike and dip Strike and dip describe the orientation of a plane in space. Strike is the bearing of a horizontal line on the plane (a scalar), i.e., N400E Dip is the inclination of the plane measured down. Dip is a vector; it gives the direction and amount of dip of the plane. Example for dip: 800N 80o is the amount, N is the direction. Example of planar structure: bedding, fault, fold axial plane, layering in lava, cleavage & schistosity.

4

5 Attitude of Beds Strike: Strike is the direction of a line formed by the intersection of the bedding plane with the horizontal plane. Strike is the bearing of a horizontal line on the inclined plane (a scalar). If a plane is immersed in a water, the strike line will be the water-line. Generally expressed as an angle relative to north. i.e. N370E, N120W

6 Attitude of Beds Dip Direction: It is the direction along which a bed dips and is perpendicular to the strike line. The dip direction is the direction that a drop of water will flow down the plane.

7 Attitude of Beds Dip: The dip of a bed is the angle between the bedding and horizontal plane, i.e., the amount of inclination with respect to horizontal. It is measured in a vertical plane at right angle to the strike of the bedding. It is expressed in degrees (450), or in gradient (1 in 1), or in percentage (50%).

8 Attitude of Beds Dip: The dip of a bed is the angle between the bedding and horizontal plane, i.e., the amount of inclination with respect to horizontal. It is measured in a vertical plane at right angle to the strike of the bedding. It is expressed in degrees (450), or in gradient (1 in 1), or in percentage (50%). HD VD d HD = Horizontal distance = 1 unit VD = Vertical Distance = 1 unit = tan d VD HD _ or, d = tan

9 Dipping Sedimentary Beds

10 Cockscomb Ridge, S. Utah Strike Dip

11 Attitude of Beds Two types of dip – a) True dip & b) Apparent dip
True dip : The angle between a bed and a horizontal plane measured in a vertical plane lying at right angles to the strike of the bedding. It is the maximum vertical angle of an inclined structural plane. It is denoted by d Apparent dip: Apparent dip is the angle measured in any direction other than the true dip direction. The amount is always less than the true dip. It is denoted by r

12 Attitude of Beds tan r = tan d sin a d = true dip r = apparent dip
a = azimuth angle between strike line and apparent dip direction The relation between the apparent dip and true dip is expressed by the following equation:- tan r = tan d sin a

13 Attitude of Beds tan r = tan d sin a d = true dip r = apparent dip
a = azimuth angle between strike line and apparent dip direction C d F a r G d Derived the equation:- tan r = tan d sin a

14 Attitude of Beds Dip & Strike Symbols Block Diagram Map View
Inclined bed Vertical bed Horizontal bed 400

15 Attitude of Beds

16 Geologic Map and Cross Section

17 Attitude of Beds Compass-clinometer for measuring strike & dip
Silva compass Brunton compass Taking a bearing of a rock feature - e.g. strike Measuring the inclination (e.g. dip)

18 Steeply Dipping Beds, Pt. Arena, Ca

19 Field Measurements

20

21

22

23 Maps and X-sections

24 Geologic Maps – strike & dip (angle, direction), geologic cross-sections

25

26

27

28 Two ways of expressing attitude
Attitude of Beds Two ways of expressing attitude N 460 N450E Amount of dip followed by dip direction W E AD DD S Strike followed by amount of dip with dip component N450W, 460 NE


Download ppt "Attitude of Beds Attitude: A general term for the orientation of a line or plane. Attitude refers to the three dimensional orientation of planar and linear."

Similar presentations


Ads by Google