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Microcline from
Strand, Østerøya, Sandefjord, Vestfold, Norway


Locality type:Pegmatite
Classification
Species:Microcline
Formula:K(AlSi3O8)
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Microcline data
Locality Data:Click here to view Strand, Østerøya, Sandefjord, Vestfold, Norway
Data Identifiers
Mindat Occurrence Record ID:773260
Long-form Identifier:1:3:773260:7
GUID (UUID V4):ea67371b-441b-4cbf-be9a-a7ac6643c941
Nearest other occurrences of Microcline
1.2km (0.7 miles) Bellavitaåsen South, Søndre Sunde, Østerøya, Sandefjord, Vestfold, Norway
1.4km (0.9 miles) Østerøyveien, Søndre Sunde, Østerøya, Sandefjord, Vestfold, Norway
1.5km (0.9 miles) Namløsholmen, Mefjorden, Sandefjord, Vestfold, Norway
1.6km (1.0 miles) Buer, Vesterøya, Sandefjord, Vestfold, Norway
1.8km (1.1 miles) Holtanskogen, Vesterøya, Sandefjord, Vestfold, Norway
1.9km (1.2 miles) Hafallen, Østerøya, Sandefjord, Vestfold, Norway
2.1km (1.3 miles) Mefjordveien, Vesterøya, Sandefjord, Vestfold, Norway
2.1km (1.3 miles) Kariåsen, Vesterøya, Sandefjord, Vestfold, Norway
2.1km (1.3 miles) Tangenbukta, Veløyveien, Vesterøya, Sandefjord, Vestfold, Norway
2.2km (1.3 miles) Husebyåsen prospect, Vesterøya, Sandefjord, Vestfold, Norway
References
Reference Search (possible matching items)
Book
book. Br0gger was able to describe eight that Norway is today a country without an academic chair in...was not possible to publish the present book in Norway. 5 ..., Introduction Alf Olav Larsen It is...Edy ( 1820). Courtesy of the National Library of Norway, picture collection. 8 The history Alf Olav...Petersburg, as well as In Italy; yes, even here in Norway it has been found. Mr. Esmarch, who on Mr. Assessor...Esmarkwasappointed asthe first professor in geologyin Norway,and moved to Christianiain 1814.Esmarkcollected
Report (issue)
with an alkaline intrusive complex. Association: Microcline, nepheline (partly altered to natrolite), fluorite...Greenland. In Norway, from the Langesundfjord area, at Brønnebukta, Siktesøya; Barkevik Strand; and the Bjørndalen...Bjørndalen quarry, Tvedalen, also at Kariåsen in the Sandefjord area. In the Burpala alkaline complex, Baikal
Journal (article/letter/editorial)
1 cm in diameter. Associated minerals include microcline, nepheline (partially altered to natrolite),...atteignant 1 cm de taille. Lui sont associés microcline, néphéline (partiellement transformée en natrolite)...with ferrokentbrooksite in the pegmatite are microcline, nepheline (partially altered to natrolite),...the Langesundfjord area, Norway (at Brønnebukta, Siktesøya; Barkevik Strand; and the Bjørndalen quarry...quarry, Tvedalen), at Kariåsen in the Sandefjord area, Norway, and in the Burpala alkaline complex, Baikal
Report (issue)
Thrusting-Zone of East-Jotunheimen 30 Trygve Strand: Sydøstligste Helgelands geologi . . . . . . 56... . . . . . . . . . . . . . . . . . 3O Trygve Strand: Sydøstligste Helgelands geologi. Med 2 tekstfigurer...Peridotite at Engenbræ, Holandsfjord, Northern Norway. With 13 textfigures. Sammendrag: Bergartene omkring...professor, dr. Leif Størmer og statsgeolog, dr. Trygve Strand har lest igjennom manuskriptet og foreslått visse...(1878, 1882, 1887), Kiær (1897, 1908), Vogt (1923), Strand (1929), Monsen (1937) og Størmer (1940, 1953),
Journal (article/letter/editorial)
Greenland; Langesundfjord area, Norway (at Brønnebukta, Siktesøya; Barkevik Strand; and the Bjørndalen quarry...quarry, Tvedalen); Kariåsen, Sandefjord area, Norway; the Burpala alkaline complex, Baikal area, Russia....in nepheline syenite. Associated minerals are: microcline, nepheline (partially altered to natrolite),
Journal (article/letter/editorial)
igneous rock-body from the Stavanger area, South Norway*) By AaILD ANDRESENand KNUTS. HEIEa, Oslo **) With...Ormakam-Moldhesten granite, from the Stavanger area, South Norway, has been dated by the Rb-Sr whole rock method...Mineralogisk-Geologisk Museum, Sarsgt. 1, Oslo 5, Norway. 260 A. ANDnESEN& K. S. HEIER- - A Rb-Sr whole...the Norwegian Caledonides, the Stavanger area (STRAND, 1960 for review of older literature, MOLLER& WURM... Given as UTM coordinates on mapsheet 1218 II, Strand. 262 A. ANDRESEN• K. S. HEIER- - A Rb-Sr whole
Report (issue)
Fault San Bernardino strand ICF rdino San Andreas Fault Wilson Creek strand GHF Mountains Mt 117...San Andreas Fault Mill Creek strand San Andreas Fault Wilson Creek strand Ba untain o Mo Pint ng Fault...Fault San Andreas Fault Mill Creek strand VT nni Fau l t MVF CHH VT 34 00' Sa n Ja c to ar...tF au tz on San Andreas Fault Mission Creek strand Litt le San Bern ardin o Mo unta 34 00' in s...zone Cucam San Andreas Fault SCF Mission Creek strand 0 es W Squaw Peak Fault 34 15' 0 lt Fau
Journal (article/letter/editorial)
origin of the Caledonian Bindal Batholith, central Norway A n n e B i r k e l a n d a, O y s t e i n N o...Trondheim, Norway bDepartment of Geology, University of Oslo, P.O.Box 1047, Blindern, 0316 Oslo 3, Norway CDepartment...origin of the Caledonian Bindal Batholith, central Norway. Lithos, 29: 257-271. The Bindal Batholith is the...Eriksons vei 39, P.O. Box 3006, Lade, 7002 Trondheim, Norway. s i d e r e d by m o s t a u t h o r s to be...Allochthon) in the east and southeast (Foslie and Strand, 1956; Ramberg, 1967; Lufro, 1979; Dallmann, 1986
Journal (volume)
1981, 1982, Taikina-aho 1982, 1983, Kangas 1985, Strand 1985, Harlna 1986,Portin 1988, Heikura 1989) and...Korkiakoski 1988, Laajoki, Strand & Harma 1989, Laajoki et al. 1983, Strand 1988). Karki and Laajoki (1990)...area and is being studied in the Jaurakka area by Strand (1985, 1988), on whose work the following description...(Reproduced from Strand 1985, Fig. 5A by the permission of the author). Photo, K. Strand. (1) The lowest...deposition at this later stage (for more details, see Strand 1985 and 1988). GeologiCal Survey of Finland"
Report (chapter)
sources for contamination of the Kara Sea. In: STRAND,P. & COOKE,A. (eds.) Proc. Intl. Conf. on ~(Environmental...~(Environmental radioactivity in the arctic,, Oslo, Norway, 21st-25th August 1995. Statens Strfilevern (Norwegian...(Norwegian Radiation Protection Authority), Osterfis, Norway, 51-56. BUGAI,D., SMITH,L. & BECKIE,R. 1996. Risk-cost...Arctic Ocean has raised some concern (Strand & Holm 1993; Strand & Cooke 1995), and the possible transport...Mineralogically, they consist of quartz, orthoclase, microcline and plagioclase feldspars, micas and hydromicas
Journal (article/letter/editorial)
in the Caledonian orogenic belt in Scotland and Norway, suggesting that the structures of both regions...Appalachians and the Caledonian belt in Scotland and Norway, thrust sheets of crystalline rocks from the core...on the southeast side of the Caledonian belt in Norway, but his hypothesis does not appear to be generally...in the Caledonian orogenic belt in Scotland and Norway. 3. PRE-CAMBRIAN ROCKS OF THE GRANDFATHER MOUNTAIN...albite, sericite, quartz, and microcline and contain porphyroclasts of microcline, sausseritized plagioclase
Journal (issue)
Mineralfunn langs ny E18 i Drammen og Nordre Vestfold Thortveititt Sc 2Si 20 7 - et historisk tilbakeblikk...Fe)-substituted anatase from Herrebl/lkasa, 0stfold, Norway..... En eksotisk pegmatitt i kambrosiluren ved... Mineralfunn Iangs ny E18 i Drallllllen og Nordre Vestfold Av Fred Steinar Nordrwn, Norsk Bergverksmusewn...amethyst, apatite, magnetite, cegirin, smoky quartz, microcline, and hyalite have been recorded together with...occurrence of unusual minerals at Bidjovagge, Northern Norway. Norges Geol. Unders. 266, 86-104. Neumann, H.
Report (volume)
gneiss of Facer Formation showing quartz and microcline in matrix of chlorite and sericite ------ 17...east of Willard Canyon. These rest on an upper strand of the Willard thrust. A second set of exposures...exposures begins as a thin wedge along the lower strand of the thrust on the ridge north of Willard City Spring...southeast to Willard Peak. Farther south along this strand of the fault only thin faulted slices are present...sequence. In the structural block just above the lower strand of the Willard thrust, the basal beds of the Huntsville
Journal (article/letter/editorial)
Pseudomorphous after biotite. In plates in pegmatite. Along strand line. In 2 in. orthoclase dike. Amethystine variety...East slope MrNtners FouNo Biotite Magnetite Microcline Orthoclase Rauetrs In the porphyry. Where microgranite...quartz veins. In conglomerate, With small garnets; strand line. Large xls. in shale. These minerals occur...ferruginous. Probably secondary, penetrating microcline. In granite porphyry. In diabasic dike. Almandite...fracture planes: purple cubes. Ilmenite Molybdenite Microcline Muscovite Pyrite Oligoclase The largest feldspar
Report (issue)
this displacement suggests that movement for one strand of the Najd faults ceased by about 560 Ma. Available...Najd fault system. Faulting along the southern strand of this system commenced in a right lateral sense...shown that left-lateral movement along the northern strand began about 670 Ma and ended about 625 Ma. Net...show that the monzogranite consists of quartz, microcline, albite, minor biotite, and trace amounts of...subsolvus and contains subequal amounts of quartz, microcline, and oligoclase. Biotite, the only mafic mineral
Journal (article/letter/editorial)
Prince Charles Mountains (Tingey 1982) and the Vestfold Hills (Oliver et al. 1982; Collerson et al. 1983)...southeast coast of Prydz Bay, depicting the Archaean Vestfold Hills and the various Proterozoic outcrops further... K-feldspar occurs both as microperthite and microcline and is commonly simply twinned. Antiperthitic...Dalkoy Is. It consists of quartz, plagioclase, microcline, microperthite and biotite. Feldspar is subhedral...intensity of D4 structures along the Brattintense S4 strand Bluffs coastline in terms of increasing S4 shear
Journal (article/letter/editorial)
calcite, e = epidote-clinozoisite, i = pyrites, m = microcline, p = plagioclase, q = quartz, s = sphene. of...quartz and microcline which are presumably of slightly later crystallization. This microcline is penetrated...emplacement; we recall the obvious splitting of microcline and the disruption of the sphenes. But it is...looking south. KING'S COLLEGE, UNIVERSITY OF LONDON, STRAND, LONDON, W.C. 2. SION. BRECCIA CORE OF THE DUNM
Journal (issue)
edition of the State Geologic Map of California (Strand, 1964). More than ninety percent of the geologic...new Weed quadrangle than on the old Weed Sheet (Strand, 1964). Some parts of the Klamaths were inaccessible... vada, California: Geology, v. 10, p. 160-166 Strand, R.G., 1964, Weed sheet, Geologic map of California:...crystals are in contact with potassium feldspar (microcline). The quartz vermicules are generally tapered...small white grain) are surrounded by light gray microcline. grain. by potassium-bearing solutions, simultaneous
Journal (article/letter/editorial)
Northwards these migmatites grade into quartzose microcline granite of the Gola island (087201) area. This...twinned and untwinned microcline, with very occasional plagioclase. Microcline Contact Relationships...enclosed by quartz. Sometimes meta-porphyroclasts of microcline ( < 1 • 3 mm.) contrast with the interstitial...descends from 350 feet O.D. to sea level at Binanea Strand (167225), the contact surface is probably nearly...80 per cent quartz, with irregular grains of microcline and basic albite (much altered to " white mica
Journal (article/letter/editorial)
Swedish part of the Caledonides by Kulling, in Strand and Kulling (1972); it has been variously interpreted...mapped from southeastern Tröndelag to northernmost Norway; they are also probably present on Atlöy (near...Bergen) and in the Egersund area of southernmost Norway; i.e. along the whole length of the mountain-belt...recrystallized sandstone contains very little feldspar (microcline). About half of the zircons in this sample are...Silvervägen (road 77 in Norway) about 10 km west of the border between Norway and Sweden. Most of the
Journal (article/letter/editorial)
mostof the rocksand is alwayssubordinate to the microcline. It forms small,wedge-shaped, straightedgedgrainsbetweenthe...as shownin Figs.8 and9, is deeplypenetratedby microcline and evenbrokenup into island-likeinclusions•vithoutany...orthoclaseis remarkably free of secondaryproducts. Microcline, the most pertinent of the rock minerals,has...resultedfrom the introductionof albite into the microcline,mostly as irregular, replacingveinlets. Some...hereandthereveinletsor stringers directedalongfracturesin the microcline (Fig. 17). Normallythegrainsin theseams andveinlets
Journal (article/letter/editorial)
228 Astrophyllite, Colorado, Greenland, Malawi, Norway, and Spain, anal., opt., isomorphous substitutions...crystal structure, 377 Barkevik, Langesundsfjord, Norway, astrophyllite, 97 Baryte, Masson Hill, Derbyshire...M6ssbauer study, anal., 448; Galway, anal., 498; Norway, anal., zI6; Spitzbergen, anal., 857; Uganda, anal...crystal structure, formula 264 Bygland, Setesdal, Norway, granite, biotite, garnet, K-feldspar, 2t6 Calabona...New South Wales, anal., hourglass zoning in, 113; Norway, complex intergrowths with orthopyroxene, 313;
Report (chapter)
part of Aust-Agder the geological map of Southern Norway is 6orninate6 by rvo, rouznlv circular oo6ieB ot...zone of fracture in the PreCambrian rocks of South Norway which runs for 150 km. from Kristiansand to Porsgrunn...specimens which bear no signs of cataclasis. Microcline "l^ne pnenocr^BrB ot microciine BQo^ rectiiinear...opric2l conrinuir^. 3ome ot tne i2rger crxBt2iB ot microcline are bor6ere6 b^ 2n irreFul2r rim ot pl2Zioci2Be...occur within the microcline. Barth (1947, p. 180) was of the opinion that the microcline in the Herefoss
Journal (article/letter/editorial)
]. F. L. Hausmann and L. von Buch travelling in Norway in the first decade of the last century. Somewhat...the region. As head of the Geological Survey of Norway (established in 1858) Kjerulf directed the preparation...see p. 377] . THE GEOLOGY OF PARTS OF SOUTHERN NORWAY. 317 igneous. Owing to subsidences of a rather... 33 · 3 4· THE GEOLOGY OF PARTS OF SOUTHERN NORWAY. 43. 44. 45. 46. 2. JIg RODE, KARL. 1930. Die...felspathic sandstone from this part of Southern Norway. Petrologically the term covers the same type of
Journal (issue)
to medium-grained, and composed essentially of microcline, oligoclase-albite, quartz, and biotite. The...formation, west end of Akinarssuaq (South Mountain). microcline is usually fresh and clear, whereas the plagioclase...banded gneiss is composed essentially of quartz, microcline, oligoclase-andesine, and brown biotite, with... sutured, and shows undulose extinction. The microcline appears very fresh, clear, and unaltered, whereas...from a mile (1.6 kros.) south of Narssårssuk. Microcline is abundant in a sample from 3 miles (4.8 kros
 
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