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12 2
2005 4
(,; )
Eart h Science Frontiers (China University of Geosciences ,Beijing ; Peking University)
Vol. 12 No. 2
Apr. 2005
1 , 2 , 1 , 3
11 , 610059
21 ,100083
31 , 210093
CH EN Xi 1 , WAN G Cheng2shan 2 , L I Xiang2hui 1 , HU Xiu2mian 3
11 College of Geoscience , Cheng du Universit y of Technolog y , Cheng du 610059 , China
21 China Universit y of Geosciences , Bei j ing 100083 , China
31 Department of Earth S ciences , N anj ing Universit y , N anj ing 210093 , China
CHEN Xi , WANG Cheng2shan , LI Xiang2hui , et al1 Characteristics and correlation of Upper Cretaceous oceanic red beds in
Alps2Carpathian area1 Ea rt h Science Frontiers , 2005 , 12( 2) :0612068
Abstract : In this paper , the Upper Cretaceous Oceanic Red Beds (CORBs) of the Alp s2Carpathian area are an2
alyzed in detail based on the previous data from publications. The data about 15 sections of CORBs are collect2
ed and carefully correlated from their ages , lithologies , paleontologies , sedimentation rates and paleoenviron2
ments. The most of the sections locate in Italy , Austria , Poland , Slovakia and Romania , respectively. CORBs
distributed in these countries are of many similar characteristics. They present from the Cenomanian in Scaglia
Bianca formation in Italy , Pustelnia marl member and Macelowa marl member in Poland , and continue to the
lower Palaeogene in Nierental formation in Austria. CORBs present in Campanian strata in all areas but Mace2
lowa marl member. Most of them are formed by limestones , marls and marly limestones. In Nierental forma2
tion they are intercalated with turbidite succession. High carbonate content ( > 50 %) and low TOC content is
the common feature of CORBs in the study area. The planktonic foraminiferas are found as main fossils in
these strata. The sedimentation rates of CORBs range from 1 4 mm/ ka ( shallow marine sediment of
Pustelnia marl member and Macelowa marl member) to 1035 mm/ ka ( Gura Belei formation , Romania) ,
which are relatively low and vary in different locations. It cannot be directly connected with sediment color.
CORBs can present either above the CCD or below. Generally , the palaeoenvironments range from continent
margin basin , continental slope to deep oceanic basin. More detailed data about CORBs are presented in this
paper as well.
Key words : Alps ; Carpathians ; Upper Cretaceous ; Oceanic Red Beds
:,
,Cenomanian ,
,Campanian , ,
,,CCD ,
,
:; ; ;
:2004 11 03 ;:2005 01 10
:(2001CCA01800) ;(40332020) ;(IGCP 463)
: (1983 - ) ,,,E2mail :chnchx @1261com
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62
, , , / ( Earth Science Frontiers) 2005 , 12 (2)
: P5341 53 ; P736122 :A :1005 2321 (2005) 02 0061 08
,
,
,
211
(cretaceous oceanic red beds ,CORBs) [1 ] ,CORBs U mbria2Marche
1860 (2 A E) [ 7 ,8 ,22 ]
Λt r ,
Campanian Bianca Scaglia Rossa [9 ] ,
P chov [2 ] [10 ]
,,
, [11 ,12 ] ,-
,10110 cm ,25 cm ,
23 cm60 m [10 ] ,
, 10 m ,
1
Ratali pora brotzeni , R. reicheli [12 ]
,,(
) () (2B) Bonarelli 4 m [14 ] ,
[ 3 ] ,Genoa ,
,
, ,
,
[4 ] ,
;
,Balkans Rhodopes , [16 ] ,K/ T
[5 ] 2050 cm [10 ]
[17 ]
Pannonian [ 4 ]
[17 ] ,
Helvetic Peninic
Pannonian met rica , G. elev at a , G. vent ricaosa , G. calcarat a ,
Magura Pieniny G. hav anensis , G. f alsost uarti , G. g ansseri , R.
Moldavides Moldavides Dacides cont usa , A . m ay aroensis G. eu g ubi na [17 ,18 ] ,
(1) Turonian
Umbria2Marche
Pieniny Go sau Nierental (2 D) ,
Pannonian ,
2
,
Scisti a Fucoidi Scaglia
Scaglia Bianca Albian2Cenomanian
,
, [10 ]
(Bonarelli ,OAE2) [13 ] ,
Cenomanian R1 cushmani
Bottaccione Scaglia
Rossa
235 m [14 ,15 ] ,
Hel vetoglobot runcana hel vetica [12 ]
H. hel vetica , M. si gali , D. concav ata , D. as y2
,
Gosau;
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, , , / ( Earth Science Frontiers) 2005 , 12 (2)
63
[4 ,6 ]
1
Fig. 1 Geological sketch of Alps2Carpat hian area
1 - Helvetic Peninic ; 2 - ; 3 - Tauren ; 4 - Pannonian ; 5 - Magura ; 6 -
Pieniny ; 7 - ; 8 - ; 9 - Krosno2Menilite Moldavides ; 10 - Moldavides ; 11
- Dacides ; 12 - Pannonian ; 13 - ;AP -
[19 ] ( Globot runcana area , G. bulloi des ,
[ 20 ,21 ] , ( marly G. f ormicate , G. elev ate )
limestone) , (B roi nsoni a p arca , Cret arhabd us conicus , C. cre2
,400 m [22 ] ,nul at us ) [15 ,25 ] , Glo2
50 % [23 ] ,cm bot runcana area [26 ]
B roi nsoni a
dm ,p arca [27 ] Coniacian2Campanian
m
,Brandenberg Santo2 Pieniny ,
nian , J aworki Pustelnia
Maastrichtian ,Campanian Macelowa (2 G N) [ 28 ]
[20 ] ;Campanian ,,
[24 ]
212
Cenomanian 2Campanian
[29 ,30 ] Pustelnia
Brezovsk,,3040 m [10 ]
Karpty Myjava (2 F) ,3 m Lorencowe ,
J ablonica ,KoΛarisk( P chov (14 cm)
) [15 ,25 ] Hurbanova Dolina ,
;
[15 ,30 ]
Macelowa
Podbradlo KoΛarisk , 2
, [15 ,29 ,30 ] ,1050 m
,50 m ,Campanian Rotali porareicheli ( Cenomanian
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64
, , , / ( Earth Science Frontiers) 2005 , 12 (2)
2
Fig. 2 Main lit hology columns of CORBs in Alps2Carpat hian area of western Tet hys
1 - ;2 - ;3 - ;4 - ;5 - ;6 - ;7 - ;8 - ;9 - ;10 -
:A - Umbria2Marche Piobbico [7 ] ;B - Bottaccione Scaglia Rossa [14 ] ;C - Ultrahelvetic
[8 ] ;D - Gosau [21 ] ; E - Rehkogelgraben [8 ] ; F - Santonian2Campanian [25 ] ; G -
Zlobowy Creek ; H - Dolina Kosarzyska ; I - Bukowiny ; J - Bukowiny ; K - Macelowa2Osice ; L - Szewc w Gronik ; M - Pod2
skalnia G ra ; N - Orlica [29 ] ; O - Ialomita [31 ]
)2Globot runcanell a hav anensis (Campanian) Bak [30 ] ,
Rot ali pora globot runcanoi des (Cenomanian )2
,
Dicari nell a as y m met rica ( Santonian ) [ 15 ,29 ,30 ] B ulbobaculites p roblem aticus , Uvi geri nam mi na
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, , , / ( Earth Science Frontiers) 2005 , 12 (2)
65
j ankoi , Goesella ru gosa ,,
Cau dam mina gi gantean
,
,Iamoli. a Praho2
va ,Gura Beliei (2 O) [31 ] [15 ]
312
Plaiu ,Prahova ,
85 % ,15 %20 % [ 30 ]
Dumbravioara 60170 m Lorencowe ,Campanian
[31 ] ,: [30 ] ,3 m ,
,(14 cm) ,
; , 72 %95 % [15 ,30 ]
Campanian2Maastrichtian Macelowa
,B elem ni2
tell a m ucronat a B elem nitell a car p at hica [32 ] cm , [15 ,29 ,30 ]
Campanian
3
311
Scaglia Bianca ,,14 mm/ ka ,
Bonarelli 13. 6 %,823 mm/ ka ,
[15 ] [30 ]
,1550
cm [10 ] Rotali pora, Helvetoglobotruncana, M arginotruncana,
,Scaglia Rossa [9 ]
Scaglia Rossa 10 %80 % ,Hedbergella, Globi gerinelloi des , Het2
50 % ,,eroheli x ,
0. 07 %0. 17 % [10 ]
20 %,(15 / ) [15 ,30 ]
,,
, [10 ,14 ] ,
[32 ]
, [ 15 ]
6. 6 mm/ ka [14 ] CCD ,
3 000 m [17 ]
Nierental ,
20 %70 %,1035 mm/ ka ,
[23 ] , [31 ] ,
60 %90 % [ 19 ]
,CCD [3335 ]
,10 % ,
10 % [19 ]
, ,
10 mm/ ka ,26 mm/ ka
Zoop hycos [19 ] ,
,CCD
Pustelnia 60 %
16 %75 % ,,3
, [ 15 ,29 ,30 ]
,8 cm
14 cm ,
Macelowa ,13 cm ,
, [15 ,29 ,30 ]
,,
Rosita
Gura Beliei ,
,,
4
,
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66
, , , / ( Earth Science Frontiers) 2005 , 12 (2)
1 Alps2Carpathian
Table 1 Correlation of the typical characteristics of CORBs in Alps2Carpathian area
w (CaCO3) / % v/ (mm ka - 1 )
Scaglia Bianca Cenomanian - - - -
Turonian
Scaglia Rossa > 50
6. 6
Nierental Santonian
5090 1026
P chov Coniacian2Campnian - - -
Pustelnia
Macelowa
Gura Beliei
Cenomanian
Campanian
Cenomanian
Santonian
Campanian
6085 14
823
1675 14
823
- 1035 -
, CCD ,
[15 ] ,CCD ,,
[42 ] Scaglia Rossa Nierental
, Pustelnia Macelowa ,
(1)
,CCD
[36 ] ,CCD ,
[ 3739 ] ,,Plantagenet ,,CCD
, [40 ] [15 ,43 ]
,Campanian
,,Campanian
Kaiho ,
100 Ma (5001 600 m)
(1 6004 000 m) ,Cenomanian ,Campanian ,
100 Ma Scaglia Bianca Cenomanian , Mace2
,Campanian lowa Santonian
[ 41 ] ,,Campanian
,
, Pustelnia
Macelowa 1
4 mm/ ka ,Gura Beliei 1035 mm/
ka ,Wagreich ,
[19 ] ,,Macelowa ,
,Gura Beliei
[17 ] ,Scaglia Rossa ,50 %,
Turonian2Santonian ,
,Campanian ,Nierental ,
,, Maastrichtian 10 % ,
15 mm/ ka ,Campanian
[ 17 ,18 ]
,50 %,
5
(1)
(2)
Scaglia Bianca ,Scaglia Rossa
,Nierental
(3) ,
10 %
(4) ,,
,
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, , , / ( Earth Science Frontiers) 2005 , 12 (2)
67
(5) CCD
CCD
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