Publications of the National research council of Canada, 1918-1938 (N.R.C. nos. 1-773)

"Supplementary list", N.R.C. nos. 774-815 (6 p. 21 cm.) inserted at end. Mimeographed.

[Ressenya del llibre Rediscovering geography: new relevance for science and society, de Rediscovering Geography Committee, National Research Council]

El llibre ressenyat pretén ser una síntesi i una avaluació de la situació de la geografia als Estats Units. Estructurat en vuit capítols, els sis primers són una anàlisi de diversos aspectes de la geografia i els dos últims expliquen quina estratègia hauria de portar-se a terme per enfortir el paper de la geografia en el món acadèmic i en la societat en general

... Algebraic numbers. Report of the Committee on Algebraic Numbers, National Research Council,

Cover-title.

Theories of magnetism. Report of the Committee on theories of magnetism of the National research council,

Mode of access: Internet.

A general survey of the present status of the atomic structure problem : report of the Committee on Atomic Structure of the National Research Council /

Cover-title.

Methane generation from human, animal, and agricultural wastes : report of an ad hoc panel of the Advisory Committee on Technology Innovation, Board on Science and Technology for International Development, Commission on International Relations, National Research Council.

Mode of access: Internet.

Bulletin of the National Research Council

Mode of access: Internet.

Report of the National Research Council.

Report year ends June 30.

A partial list of the publications of the National Research Council to January 1, 1922.

"Revised and reprinted from the Proceedings of the National Academy of Sciences [vol.] 7, 1921, pages 351-362."

Methods of testing mineral aggregates and associated materials. [Prepared for the Committee on Correlation of Research in Mineral Aggregates of the Highway Research Board, National Research Council.

In 7 divisions, 1 and 7 originally issued July 18, 1930, and Nov. 26, 1929; each division with caption title: Symposium of test methods on coarse aggregates.

National Research Council of Thailand Visit

Agenda for the National Research Council of Thailand's Visit to Florida International University on May 17 and 18, 2007.

Variable stability research aircraft. Submitted to the Panel on Acceleration Stress of the Armed Forces, National Research Council Committee on Bio-Astronautics, Woods Hole Conference, 16-24 July, 1959.

Cover title.

Petrology and textural classification of the Jericho kimberlite, northern Slave Province, Nunavut, Canada

The paper presents data on petrology, bulk rock and mineral compositions, and textural classification of the Middle Jurassic Jericho kimberlite (Slave craton, Canada). The kimberlite was emplaced as three steep-sided pipes in granite that was overlain by limestones and minor soft sediments. The pipes are infilled with hypabyssal and pyroclastic kimberlites and connected to a satellite pipe by a dyke. The Jericho kimberlite is classified as a Group Ia, lacking groundmass tetraferriphlogopite and containing monticellite pseudomorphs. The kimberlite formed, during several consecutive emplacement events of compositionally different batches of kimberlite magma. Core-logging and thin-section observations identified at least two phases of hypabyssal kimberlites and three phases of pyroclastic kimberlites. Hypabyssal kimberlites intruded as a main dyke (HK1) and as late small-volume aphanitic and vesicular dykes. Massive pyroclastic kimberlite (MPK1) predominantly filled the northern and southern lobes of the pipe and formed from magma different from the HK1 magma. The MPK1 magma crystallized Ti-, Fe-, and Cr-rich phlogopite without rims of barian phlogopite, and clinopyroxene and spinel without atoll structures. MPK1 textures, superficially reminiscent of tuffisitic kimberlite, are caused by pervasive contamination by granite xenoliths. The next explosive events filled the central lobe with two varieties of pyroclastic kimberlite: (1) massive and (2) weakly bedded, normally graded pyroclastic kimberlite. The geology of the Jericho pipe differs from the geology of South African or the Prairie kimberlites, but may resemble Lac de Gras pipes, in which deeper erosion removed upper fades of resedimented kimberlites.