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Variations in the strength of gravity occur from place to place according to the density distribution of the rocks beneath the surface. Such gravity anomalies have been mapped across the British Isles and adjacent areas〔http://www.earth.ox.ac.uk/~tony/watts/downloads/wattsfairhead97.pdf British Isles Gravity anomalies and magmatism along the western continental margin of the British Isles〕 and they reveal aspects of these islands’ geological structure.〔British Geological Survey 1997, ''Gravity Anomaly Map of Britain, Ireland and Adjacent Areas'', Smith & Edwards 1:500K〕 ==Negative Anomalies== Negative gravity anomalies are associated with local deficiencies in mass due to volumes of rock which are less dense than the average. Typically these anomalies are associated with granite plutons and with sedimentary basins. Gravity anomaly maps of the British Isles are interpreted as indicating the presence of granite plutons in the following areas. The list is not exhaustive: *Galloway *Cheviot Hills *Mountains of Mourne *Connemara *Donegal *South West England (Cornubian batholith and Haig Fras granite) *Askrigg Block (Yorkshire Dales) *Alston Block (North Pennines) *Grampian Highlands (Cairngorms etc.) The Weardale Granite, a batholith some 60 km by 25 km in extent underlying the Alston Block of the northern Pennines, was first detected by gravity survey. Drilling of the Rookhope borehole subsequently confirmed the existence of this substantial body of granite. A combination of gravity anomaly data and boreholes has permitted geologists to work out the shape of this pluton.〔Stone et al. 2010, 'British Regional Geology: Northern England' (5th Edn) British Geological Survey pp97-98〕 A further borehole was drilled at Raydale to investigate the origin of the gravity anomaly underlying the Askrigg Block. This proved the existence of the Wensleydale granite - a body of rock which is nowhere exposed at the surface.〔Aitkenhead et al. 2002, 'British Regional Geology: The Pennines & adjacent areas' (4th Edn) British Geological Survey p15〕 Similarly, negative anomalies coincide with the following sedimentary basins (amongst others): *Moray Firth Basin *North Channel Basin *Solway Basin *Kish Bank Basin *Munster Basin *Vale of Eden *Vale of Clwyd *Cheshire Basin *Worcester Graben *Hampshire Basin *Cardigan Bay Basin *St George’s Channel Basin *Wessex Basin *Rockall Basin *Porcupine Basin The negative anomaly associated with the Worcester Basin/Graben has sharp margins and is particularly pronounced. Work by researchers, Cook and Thirlaway and also by Brooks in the 1950s and 60's resulted in estimates of the thickness of the sedimentary rock sequence in the basin. Models for the structure of the basin are in part based on their interpretation of the gravity anomaly together with data from seismic surveys and a borehole at Kempsey.〔Barclay, WJ et al. 1997 'Geology of the country around Worcester, Memoir of the British Geological Survey' sheet 199 (E&W)〕 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Gravity anomalies of Britain and Ireland」の詳細全文を読む スポンサード リンク
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