M
Marie D. Jackson
Researcher at University of Utah
Publications - 47
Citations - 1742
Marie D. Jackson is an academic researcher from University of Utah. The author has contributed to research in topics: Pozzolan & Volcano. The author has an hindex of 20, co-authored 45 publications receiving 1416 citations. Previous affiliations of Marie D. Jackson include University of California, Berkeley & United States Geological Survey.
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Journal ArticleDOI
High-volume natural volcanic pozzolan and limestone powder as partial replacements for portland cement in self-compacting and sustainable concrete
Kemal Celik,Marie D. Jackson,Mauricio Mancio,Cagla Meral,A.-H. Emwas,P.K. Mehta,Paulo J.M. Monteiro +6 more
TL;DR: In this paper, a laboratory study demonstrates that high volume, 45% by mass replacement of portland cement (OPC) with 30% finely-ground basaltic ash from Saudi Arabia (NP) and 15% limestone powder (LS) produces concrete with good workability, high 28-day compressive strength (39 MPa), excellent one year strength (57 MPa) and very high resistance to chloride penetration.
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Phillipsite and Al-tobermorite mineral cements produced through low-temperature water-rock reactions in Roman marine concrete
Marie D. Jackson,Sean R. Mulcahy,Heng Chen,Yao Li,Qinfei Li,Piergiulio Cappelletti,Hans-Rudolf Wenk +6 more
TL;DR: Jackson et al. as discussed by the authors showed that Altobermorite also occurs in the leached perimeters of feldspar fragments, zeolitized pumice vesicles, and in situ phillipsite fabrics in relict pores.
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Unlocking the secrets of Al-tobermorite in Roman seawater concrete
Marie D. Jackson,S. Chae,Sean R. Mulcahy,Cagla Meral,Cagla Meral,R. Taylor,Penghui Li,Abdul-Hamid M. Emwas,Juhyuk Moon,Seyoon Yoon,Seyoon Yoon,Gabriele Vola,Hans-Rudolf Wenk,Paulo J.M. Monteiro +13 more
TL;DR: In this paper, an adiabatic thermal model of the 10 m 2 by 5.7 m Baianus Sinus breakwater from heat evolved through hydration of lime and formation of C-A-S-H suggests maximum temperatures of 85 to 97 °C.
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The laccolith-stock controversy: New results from the southern Henry Mountains, Utah
Marie D. Jackson,David Pollard +1 more
TL;DR: In this article, geologic and geophysical data and mechanical models support a laccolithic origin for the central magma chambers underlying the domes, but these data alone do not rule out the possibility of a stock at depth.