Latest Paleocene-earliest Eocene cyclostratigraphy: using core photographs for reconnaissance geophysical logging

被引:19
作者
Cramer, BS [1 ]
机构
[1] Rutgers State Univ, Dept Geol Sci, Piscataway, NJ 08854 USA
基金
美国国家科学基金会;
关键词
photographs; color; cycles; cyclostratigraphy; Paleocene; Eocene;
D O I
10.1016/S0012-821X(01)00249-7
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
I present a new method for reconnaissance cyclostratigraphic study of continuously cored boreholes: the generation of detailed sediment color logs by digitizing Ocean Drilling Program (ODP) core photographs. The reliability of the method is tested by comparison with the spectrophotometer color log for the uppermost Paleocene-lowermost Eocene section (Chron C24r) at ODP Hole 1051A. The color log generated from Hole 1051A core photographs is essentially identical to the spectrophotometer log. The method is applied to the Chron C24r section at Holes 1051A and 690B, producing the first high-resolution geophysical log for the latter section. I calculate astronomically calibrated durations between bio- and chemostratigraphic events within Chron C24r by correlating the cyclostratigraphies for Holes 1051A and 690B. These durations are significantly different from previous estimates, indicating that the chronology of events surrounding the Paleocene/Eocene boundary will have to be revised. This study demonstrates that useful geophysical logs can be generated from digitized ODP and DSDP core photographs. The method is of practical use for sections lacking high-resolution logs, as is the case for most lower Paleogene sections. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:231 / 244
页数:14
相关论文
共 37 条
[1]   Magnetostratigraphic reinvestigation of the Palaeocene/Eocene boundary interval in Hole 690B, Maud Rise, Antarctica [J].
Ali, JR ;
Kent, DV ;
Hailwood, EA .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2000, 141 (03) :639-646
[2]  
Aubry M.-P., 1996, Correlation of the early Paleogene in Northwest Europe, V101, P353, DOI [10.1144/GSL.SP.1996.101.01.18., DOI 10.1144/GSL.SP.1996.101.01.18]
[3]   Late Paleocene event chronology: unconformities, not diachrony [J].
Aubry, MP ;
Cramer, BS ;
Miller, KG ;
Wright, JD ;
Kent, DV ;
Olsson, RK .
BULLETIN DE LA SOCIETE GEOLOGIQUE DE FRANCE, 2000, 171 (03) :367-378
[4]  
Aubry MP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P37
[5]   Where should the Global Stratotype Section and Point (GSSP) for the Paleocene/Eocene boundary be located? [J].
Aubry, MP .
BULLETIN DE LA SOCIETE GEOLOGIQUE DE FRANCE, 2000, 171 (04) :461-476
[6]   Mechanisms of climate warming at the end of the Paleocene [J].
Bains, S ;
Corfield, RM ;
Norris, RD .
SCIENCE, 1999, 285 (5428) :724-727
[7]  
Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129
[8]   A SALT OSCILLATOR IN THE GLACIAL ATLANTIC? 1. THE CONCEPT [J].
Broecker, Wallace S. ;
Bond, Gerard ;
Klas, Millie ;
Bonani, Georges ;
Wolfli, Willy .
PALEOCEANOGRAPHY, 1990, 5 (04) :469-477
[9]  
Browning JV, 1996, GEOLOGY, V24, P639, DOI 10.1130/0091-7613(1996)024<0639:GIOLTM>2.3.CO
[10]  
2