Synthesis of late Paleozoic and Mesozoic eolian deposits of the ...

More documents

Recommendations

Info

117 ° 112 ° 107 ° 102 ° ' ¢ ' ' I _._-:--- \ ~z~_J~ ,, , +~ __ ,, ~--~- • =__/_ ___~'~, K- , ~ I _.-I._.. !1 J : I .',-~~.-, '~~-,~~ -~, k ~- ~ ,-G ~--- Ik~r~, ¢ L --~, --- ---t ..... 'W I ~1 , ~- i ~ i----------",-, h_l ! I j--J__L_ ~-.--r------q • ~ ~"~ -7 --~ ' ~ ~ - J-----i k.___2 I I ..._A ~'-, ..L---i ~ --'--I ', r'-"-'-I ~--3F-;-T---~ \ ,'---'---~--,~;~'~-~r~m~--:~, --" -#- + ,j _.. -~.°+~ oo.~.~1 - , , , ~ t----~~ ~. x . I I ~ ! / I / ,-~ f-----~----,---x t-'l_------ "', ~, I'--,. ~°I h ', ^/ ~ / 3 -~ ~_____ \ ,.. ~ , I _-Lrd-~, --,---- ......___ .~ I ~ -- I - ~---r-- I --~- / I ,x ~~ ~-- /~.i ~~-i _L;, / i'~k)--~_A ~-~P-- - " L. I ........ k~ ._,". r I t__ h t------ ~- I I I I I "+ ! I;0 1002;0 i ;:O;mMi "~1~. 1 I ~'~ J. "7 + + Fig. 31A. Geometry of Middle Jurassic VI eolian deposits. Isopach interval 30 m. Solid lines where outcrops occur; dashed lines where interval in subsurface or removed by erosion.
117 ° 112 107 ° 102 ° / "k'/"~ ~ -'~"1 7 / ~ i ~'1 I I I i --~---'-- -~'----- 'l. I -" ~" L~ ~_, -~ \ . r/..j _x~---,_A__X---p-- ! ""-,-kX-,_77r~O I-T t l I ~--,,----- -- ,- ,- " I I I I -L "'I-'~ I-- I I I ; ~ ~,l , I ~--L_A----4, ,--, A ~---t ~ ~ I .h-r-~, _,--,, ~ r L _ _ _ L . . . . , r' -- / / ~--T~,~-~-~ ,~ - r i~~-~ ~ , I [ .- ~. I ;~--~ , I J'~l~ IL I ~ ,____jl "I ~-_ ,l I ~. i I-----I ~ ~--~--I _L __-~- , I I LE JURASSIC I " -- L __.-..i..-~ i~ _, i-----.x...___ ' ~= !--/ - k.__~ _------ - --- \ , --~ ~ ..~.:-'~,~ , P- ~,~: ~ --7 \. I I d ~%:C",,' ! I i i ~ ~ | ~------ pp. 67-70 ~ . I I ! / I / '4, f--""~-- ~ t--L----i--- \~ I"a i , I r -~--I--~-~T " ! i --T-----Y / -'-%'. rAb~L----- ~ ----~---'---~ ~'Y-~,~: i -#--; ! 0 100 200 Mi ~---i " I i \ l /---_ | , I , , ~ i l '-.
Page 1 and 2:
Sedimentary Geology, 56 (1988) 3-12
Page 3 and 4:
method of presentation because of t
Page 5 and 6:
The presentation of each eolian-bea
Page 7 and 8:
A A' MCNTANA WYOMING I BIGHORN POWD
Page 9 and 10:
46 ° 41 o 36' 31 ° 117 ° 112 °
Page 11:
46 ° ;I , 41 ° 117 ° 112 ° ~ '
Page 15: 117 ° 112 ° #-v~ ~ + / .~.,
Page 18 and 19: 46 ° 41 ° 36 ° 31 c 117 ! ° 112
Page 21 and 22: pp. 23-26 46 ° 41 o 36 ° 31 ° 11
Page 23: - 4' 117 ° 112 ° 107 ° 102 ° '
Page 26 and 27: 28 east into the Central Colorado t
Page 28 and 29: 30 Blakey (1986) documented the pre
Page 30 and 31: 32 A WYOMING : COLOR, DO A I SOUTH'
Page 32 and 33: 34 the southern Monument Uplift and
Page 34 and 35: , 117 ° 112 ° 107 ° 102 ° 40o~
Page 37 and 38: pp. 39-42 46 ° 41 ° 36 ~ 31 c -v_
Page 39: 117 ° 112 ° 107 ° 102 ° ' ¢ '
Page 42 and 43: G (B) SOURCES OF DATA FOR MIDDLE JU
Page 45 and 46: pp. 47"50 46 ° 41 `= 36 c -=-=.=.
Page 47: 117 ° 112 ° 107 ° 102 ° ! l I
Page 50 and 51: 52 C) A ID.~HO I WYOMING NORTHERN W
Page 52 and 53: 54 during the Jurassic Period (Pete
Page 54 and 55: 56 called the "Reservation facies".
Page 56 and 57: 58 A A' WYINE NEICO WIND RIVER LARA
Page 58 and 59: 60 F F' SS AT MESITA Recopture Mbr
Page 60 and 61: 62 member is unconformably overlain
Page 62 and 63: 64 B UTAH [ ARIZONA LAKE POWELL " I
Page 64 and 65: 66 misleading. The eolian beds are
Page 69 and 70: pp. 71-74 46 ° 41 ° 36 ° 31'= 11
Page 71: ~o ~o o o o I I | I + O I I I -----
Page 74 and 75: 76 the logs so the contour lines ar
Page 76 and 77: 78 TABLE 1 Methodology used in cons
Page 78 and 79: 80 TABLE 2 (continued) Section Auth
Page 86 and 87: 88 TABLE 4 Data base for Wingate Sa
Page 98 and 99: 100 TABLE 6 (continued) Section Aut
Page 116 and 117:
118 Deposits of the Western Interio
Page 118 and 119:
120 Arizona, New Mexico, and Utah.
Page 120 and 121:
122 O'Sullivan, R.B., 1984. Stratig
Page 122 and 123:
124 Thaden, R.E., Thrites, A.F. and
show all

Synthesis of late Paleozoic and Mesozoic eolian deposits of the ...

Create successful ePaper yourself

Delete template?

Save as template?