Changing Brine Inputs Into Hydrothermal Fluids: Southern Cleft Segment, Juan de Fuca Ridge

Abstract In 2016, temperature recorders were recovered, temperatures were measured, and fluid samples were collected from Vent 1, a high temperature (338°C) hydrothermal discharge site on the southern Cleft Segment of the Juan de Fuca Ridge. Coupled with previous sampling efforts, this collection re...

وصف كامل

التفاصيل البيبلوغرافية
الحاوية / القاعدة:Geochemistry, Geophysics, Geosystems
المؤلفون الرئيسيون: C. Geoffrey Wheat, Robert A. Zierenberg, Jennifer B. Paduan, David W. Caress, David A. Clague, William W. Chadwick Jr.
التنسيق: مقال
اللغة:الإنجليزية
منشور في: Wiley 2020-11-01
الموضوعات:
Hydrothermal
brine
Cleft Segment
Juan de Fuca
mid‐ocean ridge
water‐rock reaction
الوصول للمادة أونلاين:https://doi.org/10.1029/2020GC009360

الانترنت

https://doi.org/10.1029/2020GC009360

مواد مشابهة