Zobrazeno 1 - 10
of 21
pro vyhledávání: '"Lambertus C. Struik"'
Publikováno v:
Canadian Journal of Earth Sciences. 38:657-678
New magnetic and paleomagnetic data for central British Columbia support and quantify the hypothesis that the area underwent significant Tertiary-age transtensional deformation. Paleomagnetically determined tilts in Eocene rocks indicate that four fa
Publikováno v:
Canadian Journal of Earth Sciences. 38:485-494
The Canadian Cordillera in central British Columbia has seen the Mesozoic subduction of an oceanic terrane; the amalgamation of volcanic-arc terranes; continued intermittent Mesozoic compression and magmatism; and Tertiary wrenching, extension and ma
Publikováno v:
Canadian Journal of Earth Sciences. 38:515-534
West of Prince George, British Columbia, the Cache Creek Terrane is composed of mafic lavas interlayered with both mid-Permian pelagic limestones and Upper Triassic siliceous shales and greywackes. Gabbro, basalt, dolerites, and foliated clinopyroxen
Publikováno v:
Canadian Journal of Earth Sciences. 38:603-618
The Endako low-F granodiorite-type porphyry Mo deposit is hosted by the Triassic to Eocene Endako batholith, which comprises five temporally distinct plutonic suites, only one of which is mineralized. Pre-mineralization suites range in composition fr
Publikováno v:
Economic Geology. 96:171-196
The Endako batholith is a composite batholith that consists of early foliated hornblende ± biotite diorites, intermediate-age unfoliated hornblende ± biotite diorites, and late granodiorites to monzogranites. These latter plutons host the Endako mo
Autor:
Lambertus C. Struik
Publikováno v:
Canadian Journal of Earth Sciences. 30:1262-1274
In central British Columbia, north-trending dextral strike-slip faults that cut Late Eocene granite also truncate northwest-trending dextral strike-slip faults. The northwest-trending strike-slip faults bound the Wolverine Metamorphic Complex (Wolver
Autor:
Marc Tardy, A. Narros, Anita Cadoux, Henriette Lapierre, Lambertus C. Struik, Delphine Bosch, Pierre Brunet
Publikováno v:
Canadian journal of earth sciences
Canadian journal of earth sciences, National Research Council Canada, 2003, 40, pp.833-852. ⟨10.1139/E03-010⟩
Canadian journal of earth sciences, National Research Council Canada, 2003, 40, pp.833-852. ⟨10.1139/E03-010⟩
The Slide Mountain Terrane consists of Devonian to Permian siliceous and detrital sediments in which are interbedded basalts and dolerites. Locally, ultramafic cumulates intrude these sediments. The Slide Mountain Terrane is considered to represent a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::164375063a831ddf688a3f4c6547222d
https://hal.archives-ouvertes.fr/hal-00105085
https://hal.archives-ouvertes.fr/hal-00105085
Publikováno v:
Chemical Geology
Chemical Geology, Elsevier, 2003, 201(1-2), pp.55-89. ⟨10.1016/S0009-2541(03)00224-9⟩
Chemical Geology, Elsevier, 2003, 201(1-2), pp.55-89. ⟨10.1016/S0009-2541(03)00224-9⟩
Two major Late Paleozoic–Triassic oceanic terranes are exposed in the North America Cordillera. Slide Mountain Terrane is made up of dolerites, pillow basalts associated with cumulate gabbros and peridotites ranging in age from Carboniferous to Per
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ad1f412b87f0ed771833bf95a9c77312
https://hal.archives-ouvertes.fr/hal-00105076
https://hal.archives-ouvertes.fr/hal-00105076
Autor:
Lambertus C. Struik, Henriette Lapierre, Hiroyoshi Sano, Michael J. Orchard, Marc Tardy, P. Schiarizza, Fabrice Cordey, D. G. MacIntyre
Publikováno v:
Canadian journal of earth sciences
Canadian journal of earth sciences, National Research Council Canada, 2001, 38 (4), pp.495-514. ⟨10.1139/e00-117⟩
Canadian journal of earth sciences, 2001, 38 (4), pp.495-514. ⟨10.1139/e00-117⟩
Canadian journal of earth sciences, National Research Council Canada, 2001, 38 (4), pp.495-514. ⟨10.1139/e00-117⟩
Canadian journal of earth sciences, 2001, 38 (4), pp.495-514. ⟨10.1139/e00-117⟩
International audience; Upper Paleozoic to Lower Jurassic oceanic rocks of the Cache Creek Terrane near Fort St. James, in central British Columbia, form a stack of thrust sheets cut by steeply dipping strike-slip faults. Paleontologically dated uppe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f0ce7e2c4954857c90bca9af4aedbdf8
https://hal.archives-ouvertes.fr/hal-03274755
https://hal.archives-ouvertes.fr/hal-03274755
Autor:
H. J. Taylor, E. W. Bamber, Fabrice Cordey, Lambertus C. Struik, Bernard Mamet, Hiroyoshi Sano, L. Rui, Michael J. Orchard
Publikováno v:
Canadian journal of earth sciences
Canadian journal of earth sciences, National Research Council Canada, 2001, 38 (4), pp.551-578. ⟨10.1139/e00-120⟩
Canadian journal of earth sciences, 2001, 38 (4), pp.551-578. ⟨10.1139/e00-120⟩
Canadian journal of earth sciences, National Research Council Canada, 2001, 38 (4), pp.551-578. ⟨10.1139/e00-120⟩
Canadian journal of earth sciences, 2001, 38 (4), pp.551-578. ⟨10.1139/e00-120⟩
International audience; Conodonts, radiolarians, foraminiferids, and corals provide constraints on the geology and tectonics of the Nechako region. They also support the notion that the Cache Creek Terrane is allochthonous with respect to the North A
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ca2f219a9023ef47910300bb5e381805
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=231731
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=231731