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Grotzinger and Milliken assembled author chapters for the SEPM Special Publication in 2012. They introduced the coverage of Mars sedimentology by opining that Mars is often thought of as a volcanically dominated planet; during the last decade of exploration in orbit and on the surface, these have revealed with increasing clarity the role of sedimentary processes on the Red Planet.

Data from recent orbiters have highlighted the role of sedimentary processes throughout the geologic evolution of Mars by providing evidence that such processes are preserved in a rock record that spans a period of over four billion years.

Rover observations have provided complementary outcrop-scale evidence for ancient eolian and fluvial transport and deposition, as well as surprisingly Earth-like patterns of diagenesis that involve recrystallization and the formation of concretions. In addition, the detection of clay minerals and sulfate salts on Mars, coupled with large-scale morphologic features indicative of fluvial activity, indicate that water-rock interactions were once common on the Martian surface.

No mention of one of the first serious papers on the groundwater below the surface of Mars: https://i2mconsultants.com/downloads/mdcampbell/MarsGeoHy89.pdf

Here is the coverage of those chapters that are available for download (for free):

Overview

The Sedimentary Rock Record of Mars: Distribution, Origins, and Global Stratigraphy

Authors:
John P. Grotzinger;
Ralph E. Milliken

An Atlas of Mars Sedimentary Rocks as seen by HIRISE

Authors:
Ross A. Beyer;
Kathryn M. Stack;
Jennifer L. Griffes;
Ralph E. Milliken;
Ken E. Herkenhoff;
Shane Byrne;
John W. Holt;
John P. Grotzinger

Weathering, Diagenesis, Geochemistry

Aqueous Alteration in Martian Meteorites: Comparing Mineral Relations in Igneous-Rock Weathering of Martian Meteorites and in the Sedimentary Cycle of Mars

Author:
Michael A. Velbel

Geochemistry of Sedimentary Processes on Mars

Author:
Scott M. McLennan

Sediment Transport and Deposition

Were Aqueous Ripples on Mars Formed by Flowing Brines?

Authors:
Michael P. Lamb;
John P. Grotzinger;
John B. Southard;
Nicholas J. Tosca

Source-to-Sink: An Earth/Mars Comparison of Boundary Conditions for Eolian Dune Systems

Authors:
Gary Kocurek;
Ryan C. Ewing

Duststones on Mars: Source, Transport, Deposition, and Erosion

Authors:
Nathan T. Bridges;
Daniel R. Muhs

Case Studies

Focusing the Search for Biosignatures on Mars: Facies Prediction with an Example from Acidalia Planitia

Authors:
Dorothy Z. Oehler;
Carlton C. Allen

Stratigraphic Architecture of Bedrock Reference Section, Victoria Crater, Meridiani Planum, Mars

Authors:
Lauren A. Edgar;
John P. Grotzinger;
Alex G. Hayes;
David M. Rubin;
Steve W. Squyres;
James F. Bell;
Ken E. Herkenhoff

Terrestrial Analogs

Potential Recognition of Accretionary Lapilli in Distal Impact Deposits on Mars: A Facies Analog Provided by the 1.85 Ga Sudbury Impact Deposit

Author:
Philip Fralick;
John Grotzinger;
Lauren Edgar

Early Diagenesis by Modern Acid Brines in Western Australia and Implications for the History of Sedimentary Modification on Mars

Authors:
Brenda B. Bowen;
Kathleen C. Benison;
Stacy Story

Characteristics of Terrestrial Ferric Oxide Concretions and Implications for Mars

Authors:
Marjorie A. Chan;
Sally L. Potter;
Brenda B. Bowen;
W.T. Parry;
Laura M. Barge;
Erich U. Petersen;
John R. Bowman

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