{"_id":"kALDtscsyTRoMC7yj","bibbaseid":"prinzhofer-nicolas-thebogotapeninsulanewcaledoniaapossibleoceanictransformfault-1980","author_short":["Prinzhofer, A.","Nicolas, A."],"bibdata":{"bibtype":"article","type":"article","title":"The Bogota Peninsula, New Caledonia: A Possible Oceanic Transform Fault","volume":"88","copyright":"Copyright © 1980 The University of Chicago Press","issn":"00221376","url":"http://www.jstor.org/stable/30062376","doi":"10.2307/30062376","abstract":"The northern part of the Bogota peninsula belonging to the ultramafic nappe of New Caledonia shows peculiar features drastically contrasting with those in the surrounding peridotites. Within 10-15 km the foliations rotate in azimuth and become vertical. In the center of the peninsula highly sheared peridotites extend over 3 km. From structural and petrological studies, the peninsula is interpreted as a dextral shear zone, exhibiting syntectonic injection of magmatic dikes and hydrothermal alteration. The shear motion occurred in the oceanic upper mantle at temperatures between 500°C and 900°C. The overall geometry strongly supports the interpretation of a transform fault environment.","number":"4","journal":"The Journal of Geology","author":[{"propositions":[],"lastnames":["Prinzhofer"],"firstnames":["A."],"suffixes":[]},{"propositions":[],"lastnames":["Nicolas"],"firstnames":["A."],"suffixes":[]}],"month":"July","year":"1980","pages":"387–398","bibtex":"@article{prinzhofer_bogota_1980,\n\ttitle = {The {Bogota} {Peninsula}, {New} {Caledonia}: {A} {Possible} {Oceanic} {Transform} {Fault}},\n\tvolume = {88},\n\tcopyright = {Copyright © 1980 The University of Chicago Press},\n\tissn = {00221376},\n\turl = {http://www.jstor.org/stable/30062376},\n\tdoi = {10.2307/30062376},\n\tabstract = {The northern part of the Bogota peninsula belonging to the ultramafic nappe of New Caledonia shows peculiar features drastically contrasting with those in the surrounding peridotites. Within 10-15 km the foliations rotate in azimuth and become vertical. In the center of the peninsula highly sheared peridotites extend over 3 km. From structural and petrological studies, the peninsula is interpreted as a dextral shear zone, exhibiting syntectonic injection of magmatic dikes and hydrothermal alteration. The shear motion occurred in the oceanic upper mantle at temperatures between 500°C and 900°C. The overall geometry strongly supports the interpretation of a transform fault environment.},\n\tnumber = {4},\n\tjournal = {The Journal of Geology},\n\tauthor = {Prinzhofer, A. and Nicolas, A.},\n\tmonth = jul,\n\tyear = {1980},\n\tpages = {387--398},\n}\n\n","author_short":["Prinzhofer, A.","Nicolas, A."],"key":"prinzhofer_bogota_1980","id":"prinzhofer_bogota_1980","bibbaseid":"prinzhofer-nicolas-thebogotapeninsulanewcaledoniaapossibleoceanictransformfault-1980","role":"author","urls":{"Paper":"http://www.jstor.org/stable/30062376"},"metadata":{"authorlinks":{}},"html":""},"bibtype":"article","biburl":"https://bibbase.org/zotero/moniquepaez","dataSources":["bGsBCQzaqZdRxfy7J"],"keywords":[],"search_terms":["bogota","peninsula","new","caledonia","possible","oceanic","transform","fault","prinzhofer","nicolas"],"title":"The Bogota Peninsula, New Caledonia: A Possible Oceanic Transform Fault","year":1980}