Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Philip O. Banks"'
Publikováno v:
Journal of Geophysical Research: Solid Earth. 100:24101-24110
A theoretical piezomagnetic field is calculated as a function of time and ground position for an earthquake instability model applied to moderate (M ∼ 6) earthquakes on the San Andreas fault near Parkfield, California. The instability model simulat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::723a84f0116ba8608c482f588d9b7fde
https://doi.org/10.1029/95jb02516
https://doi.org/10.1029/95jb02516
Publikováno v:
Journal of Geophysical Research: Solid Earth. 96:21575-21582
An analytical solution is obtained for the piezomagnetic field generated by a single screw dislocation and its image, representing an infinitely long vertical fault with uniform strike slip that cuts the upper or lower portion of a half-space. The so
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::df462e4eaa35b86f0dae6a58bca6c111
https://doi.org/10.1029/91jb01976
https://doi.org/10.1029/91jb01976
Autor:
J. Allen Cain, Philip O. Banks
Publikováno v:
The Journal of Geology. 77:208-220
U-Pb isotopic analyses of cogenetic zircon fractions from four granitic bodies in northeastern Wisconsin yielded the following concordia intercept ages: Amberg Granite and Newingham Granodiorite, $1,860 \pm 15 m.y.$; Hoskin Lake Granite, $1,890 \pm 1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7c5e1c877877b64730792a9ccdec8871
https://doi.org/10.1086/627422
https://doi.org/10.1086/627422
Autor:
Richard A. Heimlich, Philip O. Banks
Publikováno v:
American Journal of Science. 266:180-192
A foliated granitic complex in the north evolved contemporaneously with gneiss in the south. Small ultramafic bodies in both areas were emplaced before and after metamorphism. All are cut by younger dolerite dikes. K-Ar dates in the gneiss and granit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9833e7edc3827f8fa01cd9d42c422954
https://doi.org/10.2475/ajs.266.3.180
https://doi.org/10.2475/ajs.266.3.180
Autor:
Philip O. Banks, Nobumichi Shimizu
Publikováno v:
GEOCHEMICAL JOURNAL. 3:25-34
U-Pb isotopic analyses of zircons from two granodiorites of the Abukuma Plateau indicate a period of plutonic activity in that area approximately 110m.y. ago. Zircons from two granodiorites of the Shidara area have anomalously high 207Pb/206Pb ratios
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::26ed37ef20fff3cb00c1279e0c832771
https://doi.org/10.2343/geochemj.3.25
https://doi.org/10.2343/geochemj.3.25
Autor:
Philip O. Banks
Publikováno v:
The Gulf of Mexico and the Caribbean ISBN: 9781468485370
This paper reviews briefly what is presently known about the lithologies, distribution, and ages of basement rocks surrounding the Gulf of Mexico and Caribbean Sea. The term basement is interpreted to mean pre-Mesozoic rocks, that is, rocks whose tim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::00ddb8535cc8890f45f0c11e0c0623ca
https://doi.org/10.1007/978-1-4684-8535-6_4
https://doi.org/10.1007/978-1-4684-8535-6_4
Publikováno v:
Science (New York, N.Y.). 162(3849)
Concordia resolution of uranium-lead analyses of zircons from rocks of the Guatemalan Cordillera indicates a period of plutonism, and perhaps metamorphism, in late Paleozoic times (345 +/- 20 million years). Gneisses of the Chuacus Series yield an ag
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::df97a6ae77e6ddb8a93c7ae133fe5d53
https://pubmed.ncbi.nlm.nih.gov/17738184
https://pubmed.ncbi.nlm.nih.gov/17738184
Autor:
Leon T. Silver, Philip O. Banks
The decay constant of U^(235) has been evaluated from the radiogenic Pb^(207)/Pb^(206) ratios of several cogenetic fractions of zircon and uranothorite, analyzed by conventional mass spectrometric methods. Variation of the Pb^(206)/U^(238) apparent a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::50af4a3fd8421748e297ec2d6f3ad79d
https://resolver.caltech.edu/CaltechAUTHORS:20141111-142013966
https://resolver.caltech.edu/CaltechAUTHORS:20141111-142013966
Publikováno v:
Geological Society of America Bulletin. 86:907
The Wolf River Batholith is a large anorogenic plutonic complex in central and northeastern Wisconsin that is similar lithologically to the rapakivi massifs of Finland. Quartz monzonite, the most abundant rock type present, can be subdivided into thr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ae309bd2c5a7e5d77a57c5a27f5e0bee
https://doi.org/10.1130/0016-7606(1975)86<907:gaaotw>2.0.co
https://doi.org/10.1130/0016-7606(1975)86<907:gaaotw>2.0.co