Contaminating melt flow in magmatic peridotites from the lower continental crust (Rocca d'Argimonia sequence, Ivrea–Verbano Zone)

Antonicelli, Marta; Tribuzio, Riccardo; Liu, Tong; Wu, Fu-Yuan

doi:https://doi.org/10.5194/ejm-32-587-2020

Articles | Volume 32, issue 6

https://doi.org/10.5194/ejm-32-587-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/ejm-32-587-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 32, issue 6

Research article

|

04 Nov 2020

Research article |

| 04 Nov 2020

Contaminating melt flow in magmatic peridotites from the lower continental crust (Rocca d'Argimonia sequence, Ivrea–Verbano Zone)

Marta Antonicelli, Riccardo Tribuzio, Tong Liu, and Fu-Yuan Wu

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Jan 2023	42	10	0	52
Feb 2023	41	9	0	50
Mar 2023	43	8	0	51
Apr 2023	41	10	0	51
May 2023	45	6	0	51
Jun 2023	38	5	1	44
Jul 2023	33	4	0	37
Aug 2023	37	1	1	39
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Mar 2024	42	11	0	53
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Cumulative views and downloads (calculated since 04 Nov 2020)

Month	HTML	PDF	XML	Total
Nov 2020	134	49	2	185
Dec 2020	95	15	0	110
Jan 2021	103	16	2	121
Feb 2021	78	10	0	88
Mar 2021	89	12	1	102
Apr 2021	80	10	0	90
May 2021	78	14	0	92
Jun 2021	71	8	0	79
Jul 2021	70	5	0	75
Aug 2021	72	7	0	79
Sep 2021	74	10	0	84
Oct 2021	72	25	0	97
Nov 2021	66	18	1	85
Dec 2021	68	4	0	72
Jan 2022	70	9	1	80
Feb 2022	57	7	1	65
Mar 2022	67	8	0	75
Apr 2022	51	3	1	55
May 2022	52	7	0	59
Jun 2022	57	3	0	60
Jul 2022	53	8	0	61
Aug 2022	63	3	1	67
Sep 2022	38	4	1	43
Oct 2022	39	4	2	45
Nov 2022	49	5	0	54
Dec 2022	41	6	1	48
Jan 2023	42	10	0	52
Feb 2023	41	9	0	50
Mar 2023	43	8	0	51
Apr 2023	41	10	0	51
May 2023	45	6	0	51
Jun 2023	38	5	1	44
Jul 2023	33	4	0	37
Aug 2023	37	1	1	39
Sep 2023	37	7	1	45
Oct 2023	39	10	1	50
Nov 2023	18	0	18
Dec 2023	37	4	2	43
Jan 2024	38	0	38
Feb 2024	37	6	0	43
Mar 2024	42	11	0	53
Apr 2024	28	12	1	41

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Short summary

We present a petrological⁠–geochemical investigation of peridotites of magmatic origin from the Ivrea⁠–Verbano Zone (Italian Alps), a large-scale section of lower continental crust. The main purpose is to provide new insights into the processes governing the evolution of primitive mantle magmas. We propose that studied peridotites were formed by reaction of a melt-poor olivine-rich crystal mush, or a pre-existing peridotite, with upward-migrating melts possessing a substantial crustal component.


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Contaminating melt flow in magmatic peridotites from the lower continental crust (Rocca d'Argimonia sequence, Ivrea–Verbano Zone)

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6 citations as recorded by crossref.