scholarly journals Supplemental Material: Age and tectonic setting of the Quinebaug-Marlboro belt and implications for the history of Ganderian crustal fragments in Southeastern New England, USA

Author(s):  
G.J. Walsh ◽  
et al.

<div>Google Earth KMZ file (File S1) of sample locations from Table 5 and map showing sample locations from Figure 2 (File S2). <br></div><div><br></div><div><br></div><div><br></div><div><br></div>

2021 ◽  
Author(s):  
G.J. Walsh ◽  
et al.

<div>Google Earth KMZ file (File S1) of sample locations from Table 5 and map showing sample locations from Figure 2 (File S2). <br></div><div><br></div><div><br></div><div><br></div><div><br></div>


Geosphere ◽  
2021 ◽  
Author(s):  
Gregory J. Walsh ◽  
John N. Aleinikoff ◽  
Robert A. Ayuso ◽  
Robert P. Wintsch

Crustal fragments underlain by high-grade rocks represent a challenge to plate reconstructions, and integrated mapping, geochronology, and geochemistry enable the unravelling of the temporal and spatial history of exotic crustal blocks. The Quinebaug-Marlboro belt (QMB) is an enigmatic fragment on the trailing edge of the peri-Gondwanan Ganderian margin of southeastern New England. SHRIMP U-Pb geochronology and geochemistry indicate the presence of Ediacaran to Cambrian metamorphosed volcanic and intrusive rocks dated for the first time between ca. 540–500 Ma. The entire belt may preserve a cryptic, internal stratigraphy that is truncated by subsequent faulting. Detrital zircons from metapelite in the overlying Nashoba and Tatnic Hill Formations indicate deposition between ca. 485–435 Ma, with provenance from the underlying QMB or Ganderian crust. The Preston Gabbro (418 ± 3 Ma) provides a minimum age for the QMB. Mafic rocks are tholeiitic with trace elements that resemble arc and E-MORB sources, and samples with negative Nb-Ta anomalies are similar to arc-like rocks, but others show no negative Nb-Ta anomaly and are similar to rocks from E-MORB to OIB or backarc settings. Geochemistry points to a mixture of sources that include both mantle and continental crust. Metamorphic zircon, monazite, and titanite ages range from 400 to 305 Ma and intrusion of granitoids and migmatization occurred between 410 and 325 Ma. Age and chemistry support correlations with the Ellsworth terrane in Maine and the Penobscot arc and backarc system in Maritime Canada. The arc-rifting zone where the Mariana arc and the Mariana backarc basin converge is a possible modern analog.


2019 ◽  
Author(s):  
Gregory J. Walsh ◽  
◽  
John N. Aleinikoff ◽  
Robert P. Wintsch ◽  
Robert A. Ayuso
Keyword(s):  

2020 ◽  
Vol 94 (3) ◽  
pp. 631-636
Author(s):  
Noam Maggor

Mark Peterson's The City-State of Boston is a formidable work of history—prodigiously researched, lucidly written, immense in scope, and yet scrupulously detailed. A meticulous history of New England over more than two centuries, the book argues that Boston and its hinterland emerged as a city-state, a “self-governing republic” that was committed first and foremost to its own regional autonomy (p. 6). Rather than as a British colonial outpost or the birthplace of the American Revolution—the site of a nationalist struggle for independence—the book recovers Boston's long-lost tradition as a “polity in its own right,” a fervently independent hub of Atlantic trade whose true identity placed it in tension with the overtures of both the British Empire and, later, the American nation-state (p. 631).


PEDIATRICS ◽  
1958 ◽  
Vol 22 (5) ◽  
pp. 1016-1022
Author(s):  
Saul Krugman ◽  
Robert Ward

Dr. Krugman: Since 1953 approximately 400 cases of infectious hepatitis with jaundice have been observed at the Willowbrook State School on Staten Island. The studies to be described were carried out in collaboration with Dr. Robert Ward and Dr. Joan Giles of our staff, Dr. A. Milton Jacobs of Willowbrook State School and Dr. Oscar Bodansky of Sloan-Kettering Institute. I should like to present a progress report of our investigations which have been concerned with the prevention and natural history of infectious hepatitis at Willowbrook. (A report of these studies has recently appeared in the New England Journal of Medicine (248:407, 1958) to which the reader may refer for further details.) It had been previously reported by Stokes and associates that the administration of gamma-globulin was followed by not only a lower incidence of hepatitis but also a prolongation of the protective effect. Stokes postulated that "passive-active" immunity was responsible for this phenomenon. The epidemic of hepatitis at Willowbrook provided us with an opportunity to test this hypothesis. Effect of Gamma-globulin on the Frequency of Infectious Hepatitis. Figure 1 illustrates the course of the outbreak at Willowbrook beginning in January, 1955. As can be seen, hepatitis continued to occur at a rate of about two to three cases per week. The cases, predominantly in children, occurred in 18 buildings in the institution. In June of 1956 gamma-globulin, 0.01 ml/lb, was administered to approximately a third of the inmates of each building. The control and inoculated groups were comparable as to age and time of admission to Willowbrook.


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