Microlithon alteration associated with development of solution cleavage in argillaceous limestone: textural, trace-elemental and stable-isotopic observations-Reference-Cited by-同舟云学术

Microlithon alteration associated with development of solution cleavage in argillaceous limestone: textural, trace-elemental and stable-isotopic observations

Published:1990-01 Issue:2 Volume:12 Page:165-175
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Bhagat Snehal S.,Marshak Stephen

Publisher

Elsevier BV

Subject

Geology

Reference39 articles.

1. Carbonate Sediments and Their Diagenesis;Bathurst,1975

2. Large volume loss during cleavage formation, Hamburg sequence, Pennsylvania;Beutner;Geology,1985

3. Changes in rock fabric, trace-element content, and stable-isotope composition accompanying cleavage development during pressure-solution deformation of limestone: implications for volume-loss strain;Bhagat,1988

4. Atlas of Deformational and Metamorphic Rock Fabrics,1982

5. Isotopic standards for carbon and oxygen and correction factors for mass-spectrometric analysis of carbon dioxide;Craig;Geochim. cosmochim. Acta,1957

Cited by 6 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Deformed Vein Sets as a Record of Synmetamorphic Volume Change: Quantifying Solution Mass Transfer in Subduction‐Type Metasediments of the Del Puerto Canyon Region, Franciscan Belt, USA;Journal of Geophysical Research: Solid Earth;2022-06

2. Slab-derived origin of tremolite–antigorite veins in a supra-subduction ophiolite: the Peridotite Nappe (New Caledonia) as a case study;International Journal of Earth Sciences;2019-12-03

3. Syntectonic Mobility of Supergene Nickel Ores of New Caledonia (Southwest Pacific). Evidence from Garnierite Veins and Faulted Regolith;Resource Geology;2008-06

4. Non-volatile element and volume flux in coalesced slaty cleavage;Journal of Structural Geology;1994-04

5. Open-system, constant-volume development of slaty cleavage, and strain-induced replacement reactions in the Martinsburg Formation, Lehigh Gap, Pennsylvania;Geological Society of America Bulletin;1991-07