Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Jackie M. Kleinsasser"'
Autor:
Xuyang Meng, Jackie M. Kleinsasser, Jeremy P. Richards, Simon R. Tapster, Pedro J. Jugo, Adam C. Simon, Daniel J. Kontak, Laurence Robb, Grant M. Bybee, Jeffrey H. Marsh, Richard A. Stern
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-9 (2021)
Tectonomagmatic conditions in the Precambrian were hypothesized to be unfavorable for porphyry Cu deposit formation. Here, the authors show that metallogenic processes typify Phanerozoic porphyry Cu deposits operated by ~1.88 Ga, reflecting modificat
Externí odkaz:
https://doaj.org/article/60fafb0c2e2f4cd28c7f73596751a4d7
Autor:
Xuyang Meng, Adam C. Simon, Jackie M. Kleinsasser, David R. Mole, Daniel J. Kontak, Pedro J. Jugo, Jingwen Mao, Jeremy P. Richards
Publikováno v:
Nature Geoscience. 15:1064-1070
Autor:
Jackie M. Kleinsasser, Adam C. Simon, Brian A. Konecke, Michael J. Kleinsasser, Philipp Beckmann, François Holtz
Publikováno v:
Geochimica et Cosmochimica Acta. 326:1-16
Autor:
Jeffrey Marsh, Daniel J. Kontak, Adam C. Simon, Pedro J. Jugo, Jeremy P. Richards, Jackie M. Kleinsasser, Xuyang Meng, Richard A. Stern
Publikováno v:
Journal of Petrology. 62
Most known porphyry Cu ± Au deposits are associated with moderately oxidized and sulfur-rich, calc-alkaline to mildly alkalic arc-related magmas in the Phanerozoic. In contrast, sodium-enriched tonalite–trondhjemite–granodiorite–diorite (TTG)
Autor:
Grant M. Bybee, Simon Tapster, Jeffrey Marsh, Pedro J. Jugo, Laurence J. Robb, Adam C. Simon, Jeremy P. Richards, Daniel J. Kontak, Xuyang Meng, Jackie M. Kleinsasser, Richard A. Stern
Publikováno v:
Nature Communications
Nature Communications, Vol 12, Iss 1, Pp 1-9 (2021)
Nature Communications, Vol 12, Iss 1, Pp 1-9 (2021)
Most known porphyry Cu deposits formed in the Phanerozoic and are exclusively associated with moderately oxidized, sulfur-rich, hydrous arc-related magmas derived from partial melting of the asthenospheric mantle metasomatized by slab-derived fluids.
Autor:
Martin Reich, Rodrigo Pérez-Moreno, Sebastian Held, Linda Daniele, Diego Morata, Jackie M. Kleinsasser
Publikováno v:
Applied Geochemistry. 128:104953
In the present study, we combined stable isotopes and anthropogenic tracers to investigate the origin, residence times, and evolution of thermal waters in the Lonquimay-Tolhuaca Volcanic Complex (LTVC) of the southern Chilean Andes. A total of 20 wat