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Results: 1-10 |
Results: 10
NORTH-ATLANTIC ICE-SHEET FLUCTUATIONS 10,000-70,000 YR AGO AS INFERRED FROM DEPOSITS ON THE REYKJANES RIDGE, SOUTHEAST OF GREENLAND
Authors: LACKSCHEWITZ KS BAUMANN KH GEHRKE B WALLRABEADAMS HJ THIEDE J BONANI G ENDLER R ERLENKEUSER H HEINEMEIER J
Citation: Ks. Lackschewitz et al., NORTH-ATLANTIC ICE-SHEET FLUCTUATIONS 10,000-70,000 YR AGO AS INFERRED FROM DEPOSITS ON THE REYKJANES RIDGE, SOUTHEAST OF GREENLAND, Quaternary research, 49(2), 1998, pp. 171-182
THE DEEP-STRUCTURE OF A SEA-FLOOR HYDROTHERMAL DEPOSIT
Authors: ZIERENBERG RA FOUQUET Y MILLER DJ BAHR JM BAKER PA BJERKGARD T BRUNNER CA DUCKWORTH RC GABLE R GIESKES J GOODFELLOW WD GROSCHELBECKER HM GUERIN G ISHIBASHI J ITURRINO G JAMES RH LACKSCHEWITZ KS MARQUEZ LL NEHLIG P PETER JM RIGSBY CA SCHULTHEISS P SHANKS WC SIMONEIT BRT SUMMIT M TEAGLE DAH URBAT M ZUFFA GG
Citation: Ra. Zierenberg et al., THE DEEP-STRUCTURE OF A SEA-FLOOR HYDROTHERMAL DEPOSIT, Nature, 392(6675), 1998, pp. 485-488
PHYSICAL-PROPERTIES OF REYKJANES RIDGE SEDIMENTS AND THEIR LINKAGE TOHIGH-RESOLUTION GREENLAND ICE-SHEET PROJECT 2 ICE CORE DATA
Authors: MOROS M ENDLER R LACKSCHEWITZ KS WALLRABEADAMS HJ MIENERT J LEMKE W
Citation: M. Moros et al., PHYSICAL-PROPERTIES OF REYKJANES RIDGE SEDIMENTS AND THEIR LINKAGE TOHIGH-RESOLUTION GREENLAND ICE-SHEET PROJECT 2 ICE CORE DATA, Paleoceanography, 12(5), 1997, pp. 687-695
COMPOSITION AND ORIGIN OF VOLCANIC ASH ZONES IN LATE QUATERNARY SEDIMENTS FROM THE REYKJANES RIDGE - EVIDENCE FOR ASH FALLOUT AND ICE-RAFTING
Authors: LACKSCHEWITZ KS WALLRABEADAMS HJ
Citation: Ks. Lackschewitz et Hj. Wallrabeadams, COMPOSITION AND ORIGIN OF VOLCANIC ASH ZONES IN LATE QUATERNARY SEDIMENTS FROM THE REYKJANES RIDGE - EVIDENCE FOR ASH FALLOUT AND ICE-RAFTING, Marine geology, 136(3-4), 1997, pp. 209-224
EVIDENCE FOR TOPOGRAPHY-CONTROLLED AND CURRENT-CONTROLLED DEPOSITION ON THE REYKJANES RIDGE BETWEEN 59-DEGREES-N AND 60-DEGREES-N
Authors: LACKSCHEWITZ KS ENDLER R GEHRKE B WALLRABEADAMS HJ THIEDE J
Citation: Ks. Lackschewitz et al., EVIDENCE FOR TOPOGRAPHY-CONTROLLED AND CURRENT-CONTROLLED DEPOSITION ON THE REYKJANES RIDGE BETWEEN 59-DEGREES-N AND 60-DEGREES-N, Deep-sea research. Part 1. Oceanographic research papers, 43(11-12), 1996, pp. 1683-1711
LATE QUATERNARY SEDIMENTATION ON THE MID-ATLANTIC REYKJANES RIDGE - CLAY MINERAL ASSEMBLAGES AND DEPOSITIONAL ENVIRONMENT
Authors: GEHRKE B LACKSCHEWITZ KS WALLRABEADAMS HJ
Citation: B. Gehrke et al., LATE QUATERNARY SEDIMENTATION ON THE MID-ATLANTIC REYKJANES RIDGE - CLAY MINERAL ASSEMBLAGES AND DEPOSITIONAL ENVIRONMENT, Geologische Rundschau, 85(3), 1996, pp. 525-535
REFLECTION OF SCANDINAVIAN ICE-SHEET FLUCTUATIONS IN NORWEGIAN SEA SEDIMENTS DURING THE PAST 150,000 YEARS
Authors: BAUMANN KH LACKSCHEWITZ KS MANGERUD J SPIELHAGEN RF WOLFWELLING TCW HENRICH R KASSENS H
Citation: Kh. Baumann et al., REFLECTION OF SCANDINAVIAN ICE-SHEET FLUCTUATIONS IN NORWEGIAN SEA SEDIMENTS DURING THE PAST 150,000 YEARS, Quaternary research, 43(2), 1995, pp. 185-197
VOLCANICLASTIC SEDIMENTS FROM MIDOCEANIC KOLBEINSEY RIDGE, NORTH OF ICELAND - EVIDENCE FOR SUBMARINE VOLCANIC FRAGMENTATION PROCESSES
Authors: LACKSCHEWITZ KS DEHN J WALLRABEADAMS HJ
Citation: Ks. Lackschewitz et al., VOLCANICLASTIC SEDIMENTS FROM MIDOCEANIC KOLBEINSEY RIDGE, NORTH OF ICELAND - EVIDENCE FOR SUBMARINE VOLCANIC FRAGMENTATION PROCESSES, Geology, 22(11), 1994, pp. 975-978
GEOCHEMISTRY OF SURFACE SEDIMENTS FROM THE MIDOCEANIC KOLBEINSEY RIDGE, NORTH OF ICELAND
Authors: LACKSCHEWITZ KS WALLRABEADAMS HJ GARBESCHONBERG D
Citation: Ks. Lackschewitz et al., GEOCHEMISTRY OF SURFACE SEDIMENTS FROM THE MIDOCEANIC KOLBEINSEY RIDGE, NORTH OF ICELAND, Marine geology, 121(1-2), 1994, pp. 105-119
LATE QUATERNARY CALCIUM-CARBONATE SEDIMENTATION AND TERRIGENOUS INPUTALONG THE EAST GREENLAND CONTINENTAL-MARGIN
Authors: BAUMANN KH LACKSCHEWITZ KS ERLENKEUSER H HENRICH R JUNGER B
Citation: Kh. Baumann et al., LATE QUATERNARY CALCIUM-CARBONATE SEDIMENTATION AND TERRIGENOUS INPUTALONG THE EAST GREENLAND CONTINENTAL-MARGIN, Marine geology, 114(1-2), 1993, pp. 13-36
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