Page 326 - Whole Earth Geophysics An Introductory Textbook For Geologists And Geophysicists

309
Exercises
EXERCISES
DRS direction, cutting south-north a in drawn is 9.11b Fig. in profile anomaly magnetic The 9-1 total the plot and field induced the of section cross a lines. Sketch field induced across DN5 profile. east-west an for anomaly field the 9.13, assuming Fig. in models two the for profiles magnetic and gravity the Redraw 9-2 DR4 at: occur features equator; magnetic the a) p
polarities iti i ensme: Dee Terrane i= 60° lati
; Ww ueYied youq reversed normal-polarity zone i Place magnetic differing oe rock the
Northeast stratigraphic sections of Himalayan squares) and ° i er twa nse Pakistan,” ce) eee In 30° past at : latitude at which

icy? id between (1992), the ns s the
aw sal = eezaececp ten from circ! boundary bound allowi pote Butler in in formed to

taken polarities (filled circles and ed The The ity. locality. line, time Miocene deposits of northern Pal redrawn as within rock a ithi higher magnetic to a . . is thus a clue

Interpretation ee Stratigraphy. Samples were i Paleomagnetic normal i were determined for each df million-vear-old fluvial systems in in Mi © 1982. Figure of mz agnetization izati rock drifts the when ee inclination . * paleomagnetic

Magnetic —— wy <* recduuan Paving tye Peet n anaes. Anaenas ie Neat mf 810 i istan, a gles) presents an 8.1 of inclination ; retained is S The

9 Southwest den 6 see a OR and L. Tauxe, Sedimentology, vol. 29, pp. 331-352, of i Direction Direction (i) en os - present field.
Chapter 624 ee bate fuendideagne wien tivenssipMahhy oe sedimentary deposits. From “Isochronous ; (Cross Sectional View) a) a) ° $ art

308 wy ube 9.24
d FIGURE ' eae Q erie
10 20 30 40 1
Fl eid