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Formation of dendritic crystal structures in thin silicon films on silicon dioxide by carbon ion implantation and high intensity large area flash lamp irradiation

Autor: E.H. Liepack, Wolfgang Skorupa, R. Endler, T. Gebel, Th. Schumann, Arndt Mücklich, A. Peeva, Matthias Voelskow, Xin Ou

Publikováno v: Journal of Crystal Growth 388(2014), 70-75

In this paper, we use large area light pulse induced melting of deposited thin silicon films on oxidised silicon wafers to prepare coarse grained dendritic crystal structures. The results show that the addition of carbon prevents the agglomeration of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b7936f3a1b6a432e4e3b3ff13cb8e6a4
https://doi.org/10.1016/j.jcrysgro.2013.11.057

Physical properties of Reykjanes Ridge sediments and their linkage to high-resolution Greenland Ice Sheet Project 2 ice core data

Autor: R. Endler, W. Lemke, Jürgen Mienert, Klas Lackschewitz, Matthias Moros, H.-J. Wallrabe-Adams

Publikováno v: Paleoceanography. 12:687-695

Five gravity cores taken from the Reykjanes Ridge have been used to establish a link between sediment physical properties and atmospheric records documented by δ18O variations in Greenland ice cores over the last 45,000 calendar years. Marine Gamma

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::ad25990cc7a85d7ffb37de4caf5e3948
https://doi.org/10.1029/97pa02030

Evidence for topography- and current-controlled deposition on the Reykianes Ridge between 59°N and 60°N

Autor: Jörn Thiede, B Gehrke, Klas Lackschewitz, R. Endler, Hans-Joachim Wallrabe-Adams

Publikováno v: Deep Sea Research Part I: Oceanographic Research Papers. 43:1683-1711

Sediment patterns derived from sediment sampling and acoustic subbottom profiling were mapped on the Reykjanes Ridge (North Atlantic) between 59°N and 60°N. Five discrete sediment echo patterns were distinguished and mapped on a regional scale. The

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::98e419bf80d3bc9472054a78c2699ef1
https://doi.org/10.1016/s0967-0637(96)00090-8

Late Holocene environment and climatic changes in Ameralik Fjord, Southwest Greenland - evidence from the sedimentary record

Autor: Antoon Kuijpers, Karin G. Jensen, Naja Mikkelsen, Marit-Solveig Seidenkrantz, Steffen Aagaard-Sørensen, Maarten A. Prins, R. Endler, H. S. Møller

Publikováno v: Møller, H S, Jensen, K G, Kuijpers, A, Aagaard-Sørensen, S, Seiedenkranz, M-S, Prins, M A, Endler, R & Mikkelsen, N 2006, ' Late Holocene environment and climatic changes in Ameralik Fjord, Southwest Greenland-evidence from the sedimentary record. ', The Holocene, vol. 16, no. 5, pp. 685-695 . https://doi.org/10.1191/0959683606hl963rp
Møller, H S, Jensen, K G, Kuijpers, A, Aagaard-Sørensen, S, Seidenkrantz, M S L S, Endler, R, Prins, M & Mikkelsen, N 2006, ' Late-Holocene environment and climatic changes in Ameralik Fjord, southwest Greenland: evidence from the sedimentary record ', The Holocene, vol. 16, no. 5, pp. 685-695 .
Aarhus University
The Holocene, 16(5), 685-695. SAGE Publications Ltd

Sedimentological and geochemical (XRF) data together with information from diatom and benthic foraminifera records of a 3.5 m long gravity core from Ameralik fjord, southern West Greenland, is used for reconstructing late Holocene environmental chang

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7e7ac7627386698e041354b085296f88
https://hdl.handle.net/1871.1/53d10743-7346-4366-9e8a-79aad6dcd2e2