West Lothian volcanic center

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Series: GSA Special Papers
Published: 01 January 1990
DOI: 10.1130/SPE244-p13
... associated with the West Lothian volcanic center, only 5 km to the northwest. Silica was probably precipitated by acidification when such waters entered a very local, fresh-water lake. At the same time, calcium carbonate was precipitated from surface water, due to an increase in temperature and reduction...
Journal Article
Published: 01 March 2011
Journal of the Geological Society (2011) 168 (2): 547-557.
... a ) and other traits of their primary body. Most of these taxa occur in well-drained environments, often in areas with volcanic activity, which suggests that they might have adapted more successfully to dry and/or disturbed conditions than other plant groups. Stage 4 (Early to Middle Pennsylvanian...
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Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP465.23
EISBN: 9781786203656
... that was to dominate the West Lothian region of Scotland for much of the next century, and his patented technology was eventually adopted by many early commercial oil refineries worldwide ( Carruthers et al. 1927 ; Conacher 1928 ; Dean 2018 ). Over the next 100 years, an estimated 75 MMbbl (million barrels...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1963
AAPG Bulletin (1963) 47 (7): 1294-1347.
... exploratory wells were drilled in Ireland and Belgium. The most important developments of 1962 in the Soviet Union were the discovery of oil in commercial quantities in the Lower Cambrian in central Siberia and 3 additional oil fields in the Lower Cretaceous in the West Siberian lowland. A large gas discovery...
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Journal Article
Journal: Palynology
Published: 01 January 2005
Palynology (2005) 29 (1): 23-47.
... below the Garleton Hills Volcanic Formation in the British Geological Survey (BGS) Spilmersford Borehole, East Lothian. The reference section for the Pu–TC boundary was located in the BGS Marshall Meadows Borehole, Northumberland whilst the reference sections for the TC–NM and NM–VF miospore biozones...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1932
AAPG Bulletin (1932) 16 (8): 837-858.
... of volcanic ash. The age is late Tertiary or early Quaternary. It is believed that a low-angled thrust fault has brought the igneous rocks from the west over the Guaduas beds of Upper Eocene age. Uptilted oil sands of Eocene age probably allow the oil to seep up through the igneous rock into the flat Hondo...
Journal Article
Published: 01 October 1999
Journal of the Geological Society (1999) 156 (5): 869-888.
... possible geological implications of its high density Icarus 1978 34 512 536 McGill R.A.R. Hall A.J. Fallick A.E. Boyce A.J. The palaeo-environment of East Kirkton, West Lothian, Scotland: stable isotope evidence from silicates and sulphides Transactions of the Royal Society...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1948
AAPG Bulletin (1948) 32 (7): 1292-1330.
... the section runs almost straight for 2,700 feet in the direction S. 35° W., except for the Cipero Nose, a blunt but conspicuous spur of massive marl centered at 900–1,000 feet from the end of the sea-wall. In the southern part near the point indicated there is a marked swing eastward, so that the last 800...
Journal Article
Journal: PALAIOS
Published: 01 December 2002
PALAIOS (2002) 17 (6): 571-590.
... volcanic activity” ( Anderson et al., 1999 , p. 153; parentheses by original authors). This blank now is being filled with an analysis and synthesis of plant assemblages from the middle of the Carboniferous of Gondwana that belong to neither of the aforementioned floras. These specific floras...
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