IMPACT STRUCTURE, DEVON ISLAND: IMPLICATIONS FOR THE SEARCH FOR BIOMARKERS ON MARS. J. Parnell, G.R. Osinski, P. Lee, C. S. Cockell, C.W. Taylor, Dept. of Geology & Petroleum Geology, University of Aberdeen, Aberdeen AB24 3UE, U.K., [email protected], Dept. of Geology, University of Arizona, U.S.A., Mars Institute and SETI Institute, NASA Ames Research Center, Moffett Field, CA 94035-1000, U...

Department of Science and Technology, College of Arts and Sciences, Bryant University, Smithfield, RI 02917, USA b State Key Laboratory of Loess and Quaternary Geology, IEE, CAS, Xi’an 710075, PR China c School of Human Settlement and Civil Engineering, Xi’an Jiaotong University, Xi’an 710049, PR China d LPS, Nanjing Institute of Geology and Palaeontology, CAS, Nanjing 210008, PR China Departme...

1 Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, 100029 Beijing, China 2 Shandong Institute and Laboratory of Geological Sciences, 250013 Jinan, China 3 Nansen-Zhu International Research Center, Institute of Atmospheric Physics, Chinese Academy of Sciences, 100029 Beijing, China 4 State Key Laboratory of Loess...

INTRODUCTION The Barketille subterrane is part of the peri-cratonic Kootenay termne, deposited along the western edge of ancestral North America. The Kooteoay temme, and possible correlative rocks of northern British Columbia and Yukon, contain numc~ous volcanogenic massive solphide deposits, concentrated largely in EoCambrian to Early Cambrian and Middle Devonian to Early Mississippian times. ...

The east ern Bella Coola (NTS 093D) and south ern Whitesail Lake (NTS 093E) 1:250 000 map ar eas com prise a re gion of rug ged moun tain ous to pog ra phy and lim ited ac cess on the east ern mar gin of the Coast Moun tains. These map ar eas strad dle the tran si tion zone be tween the Coast and Intermontane morphogeological belts, and en com pass the bound ary be tween ig ne ous and meta mor ...

Gcological mapping in I993 espandcd 1991 rcconnaissancc suncys ofNTS map shccts 104W12 and 13 (Smith and Mihalynuk. 1992; Figurc I). Mapping of both quadranglcs was complctcd at 1:SO 000 scale during a 2-wcck ficld scason in 1992 and a 7-wcck ficld scason in 1993. aidcd by compilation ofprcvious industry work in 10-1W12. Clbicctives of 1993 fieldwork includcd: Dc1crmin;llion oltlrc agc(s). rcgi...

(1) Laboratory for Hydrogeology, Department of Geology-Geography, Faculty of Exact Science, Catholic University of Leuven, Redingenstraat 16, 3000 Leuven, Belgium (2) Department of Hydrogeology and Engineering Geology, University of Miskolc, Miskolc, Hungary (3) Hydrogeology and Environmental Geology, Department of Georesources, Geotechnologies and Building Materials (GEOMAC), University of Liè...

Brittle and Ductile Deformational Structures in Tectonic Zones: The Research Trends in India N MANDAL1*, A CHATTOPADHAYAY2, H B SRIVASTAVA3, T K BISWAL4 and S BOSE5 1Department of Geological Sciences, Jadavpur University, Kolkata 700 032, India 2Department of Geology, University of Delhi, Delhi 110 007, India 3Department of Geology, Banaras Hindu University, Varanasi 221 005, India 4Department ...

This paper proposes a novel framework for mining regional co-location patterns with respect to sets of continuous variables in spatial datasets. The goal is to identify regions in which multiple continuous variables with values from the wings of their statistical distribution are co-located. A co-location mining framework is introduced that operates in the continuous domain without and which vi...

3D seismic data acquisition brought a sea change in subsurface imaging. The bridge between geology and seismic is P/S wave velocity of different subsurfaces/lithology. The technique has acquired prime importance due to its inherent strength of determining seismic velocity/amplitudes of the different medium. Lithological variations estimations is possible due to proper Vp/Vs ratio or either velo...