A
Iceberg scour
B
C
D
Fig.11: Depositional architecture and sedimentary facies of the Coppenbrügge subaqueous fan. A) Coarse-grained upper fan deposits, unconformably overlain by finer-grained outer- to mid-fan deposits recording a rapid ice-margin retreat and deposition on the back-slope of the abandoned fan. Note iceberg scour on top of the abandoned fan. B) Close-up view of fine-grained lower-fan deposits with ball and pillow structures, indicating high sedimentation rates. C) Close-up view of climbing-ripple cross-laminated sand; ripples migrate upslope. D) Close-up view of the iceberg scour on top of the abandoned fan. The scour is approximately 1.5 m deep and up to 1.5 m wide. Abb. 11: Architektur und Sedimentfazies des subaquatischen Coppenbrügge Fächers. A) Grobkörnige Ablagerungen des oberen Fächers, werden diskordant von feinerkörnigen Ablagerungen des äußeren und mittleren Fächers überlagert. Dies zeigt einen schnellen Eisrückzug an, der mit Ablagerungen auf dem rückseitigen Hang des verlassenen Fächers verbunden war. Am Top des Fächers ist eine Eisberg-Erosionsstruktur zu sehen. B) Nahaufnahme der feinkörnigen Ablagerungen des äußeren Fächers mit Ball- und Kissenstrukturen, die hohe Sedimentationsraten anzeigen. C) Nahaufnahme der sandigen Ablagerungen mit Kletterrippeln. Die Kletterrippeln migrieren hangaufwärts. D) Nahaufnahme der Eisberg-Erosionsstruktur am Top des Fächers. Die Erosionsstruktur ist etwa 1,5 m tief und bis zu 1,5 m breit.
core are distinctly coarse grained with relatively few sand or silt beds. Beds mainly consist of cross-bedded clast-supported pebble- to cobble-sized gravel with a fine- to coarsegrained sand matrix, which may contain scattered clasts of diamicton. Beds are often highly scoured. This coarsegrained cross-bedded upper fan gravel is interpreted to represent mouth-bar clinoforms indicating rapid deposition and progradation at an ice-marginal conduit. Deposits are texturally mature and therefore mainly represent resedimented outwash material. Slope failure and renewed sediment discharge from the tunnel mouth fed gravity flows that transported sediments radially away from the margin. Deposits of the mid-fan slope consist of massive, planar-parallel stratified, or cross-stratified pebbly sand and climbing-ripple cross-laminated sand alternating with channelized massive or normally graded gravel and pebbly sand. Towards the distal mid-fan and outer-fan slope multiple stacked climbing-ripple-cross-laminated sand units or alternations of finegrained sand, silt, and mud occur, in which individual beds 224
fine upwards. Scattered pebbles can frequently be observed and are mainly concentrated in mud layers. The lack of subaerial topset facies demonstrates that the retreat was probably fast and that fans did not reach the contemporary waterlevel (Winsemann, Asprion & Meyer 2007). Internal deformation pattern The deformation of the Coppenbrügge fan deposits includes both contractional and extensional structures. The lowermost fan is characterized by eastward dipping thrusts, recording glaciotectonic deformation of previously deposited ice-margin sediments (Winsemann, Asprion & Meyer 2004). Most commonly normal faults are developed. As in the Porta complex, normal faults are developed within the fan deposits and large-scale channel-fills show high-angle synsedimentary normal faults, which are parallel to the channel-margins and are interpreted as gravitational deformation (e.g., Clark & Pickering 1996, Moretti et al. 2003).
E&G / Vol. 60 / No. 2–3 / 2011 / 212–235 / DOI 10.3285/eg.60.2-3.01 / © Authors / Creative Commons Attribution License