ICDPLogo.gif Gas Hydrate Research Well Program
Additional Pictures
Date: 2002.02.18

ActProLogo.gif



THUMBNAIL NAME REMARKS DEPTH (m)
UN_drillsite_36.jpg Wireline DTS-Log (Distributed Temperature Sensing) with P/T-Tool at Mallik3L-38 well hole. The temperature throughout the depth of the central production well and two lateral observation wells is recorded with the distributed temperature sensors. n.a. - n.a.
UN_drillsite_37.jpg Camp staff at the Mallik Rig n.a. - n.a.
UN_drillsite_38.jpg Ernst Huenges (GFZ) and the Coiled-Tubing Rig n.a. - n.a.
UN_drillsite_39.jpg The last day of core description, sampling and analysis in the core trailer at the Mallik5L-38 well. n.a. - n.a.
UN_drillsite_40.jpg A whole core run on the preparation table in the core trailer. n.a. - n.a.
UN_drillsite_41.jpg Test for the presence of gas hydrate. In water the sediment warms up very fast and degases the methane. The result are the characteristic bubbles. n.a. - n.a.
UN_pingo_1.jpg Pingo in the Tundra in the near of the Mallik drill site. n.a. - n.a.
UN_pingo_2.jpg Detailed view of a Pingo in the near of the Mallik drill site. The Pingo is formed by an underlying ice lens covered by soil. n.a. - n.a.
UN_pingo_3.jpg Pingo n.a. - n.a.
UN_pingo_4.jpg An ice lens pushed up the overlying sediments and formed the Pingo. n.a. - n.a.
UN_pingo_5.jpg Distant view to the Mallik drill site. n.a. - n.a.
UN_pingo_6.jpg Romantics in the Tundra n.a. - n.a.
UN_pingo_7.jpg Snowman in the Tundra or prehistoric mammoth? n.a. - n.a.