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Whether a book is in the public domain may vary country to country. In the young Mugil referred to the bone was doubtless lost in preparing the skeleton, for I find it well developed in much smaller individuals that those re- ported upon. The upper part of the sheet of tendon is free from the muscle and at its anterior end helps to form the maxillary tendon. He suggests* that the different minerals which make up the sulfid *Daly, R. — Igneous rocks and their origin, 454 (1914)- ^Die Erzlagerstatten der Nutzbaren Mineralien und Gesteine, 1, 240 (1910). INTRODUCTION 7 matte are mutually immiscible, and the sulfids last to crystallize intrude the previously solidified sulfids. Our study of the magmatic ores has led us to frame the hypothe- sis that the magmatic ores in general have been introduced at a late magmatic stage as a result of mineralizers, and that the ore-minerals replace the silicates.

Public domain books are our gateways to the past, representing a wealth of history, culture and knowledge that's often difficult to discover. Volume, Papers by John Emat Matzlte, tat3 Professor of Romanic [.anguages. It has seemed most convenient for the needs of this paper to follow no scheme of grouping. Continuous with this sheet of tendon is the tendinous covering of the inferior part of the adductor mandibulae, or the part confined to the mandible (A-co of Vetter), which posteriorly sends back a bundle of fibers to the middle of the quadrate. •Howe, R — Petrographical notes on the Sudbury nickel deposits. This replacement, however, differs from that caused by destructive pneumatolytic or hydrothermal processes in that quartz and secondary silicates are not formed at the time the ores are deposited.

You can search through the full text of this book on the web at |http : //books . com/| m.ohikh; USMURY LELAND STANFORD JUNIOR UNIVERSITY PUBUCATIONS — IJNIVHRSITV SF. The Friday Mine, San Diego County, California 39 Microscopic description; Summary. Part three contains a brief summary of our conclusions and a statement of the criteria by which the magmatic ores may be recog- nized. The conclusions we have reached in regard to the origin of the ores, and to the order of sequence of the ore-minerals, appear to us to have a broader application than to nature's processes of igneous metallurgy. (2) As a result of the crystal- lization and removal of the mafic minerals, there is a concen- tration in the still fluid magma of the felsic constituents, of gases and of mineralizers, of those elements (chiefiy the precious and base metals) the crystallization of which is delayed by mineralizers (chlorin, fiuorin, boron, water, hydrogen sulfid, etc.). If so, the two types of ore will be concentrated at different places, one at the base of the intrusive magma and the other near its upper and outer margins. 12 A STUDY OF THE MAGMATIC SULFID ORES of solubility in anhydrous melts, or are the relations more compli- cated?

HIES he Sesamoid Articular A Bone in the Mandible of Fishes Edwin Chapin Starks Asslstanl Prolessor of Zoology WITH RFTBEN TEXT FIGURES STANFORD l/MVERSITY, CALIFORNIA PUBLISHED BY THfc UNIVERSITY igi6 UNIVERSITY SERIES 'ftfftf BRITAif CB IN Silkworms, I. The Golden Curry Mine, Montana 41 Geology; Microscopic description. * The second subdivision of the magmatic sulfid ores was suggested by Stutzer [Zcit f. Geol., 15, 311 (1907)] and the importance of the group was estab- lished by the detailed descriptions of the productive deposits in Little Namaqua- land [Rogers, A. : The nature of the copper deposits of little Namaqualand. Altho magmatic ore segregations are merely uncommon rock types,' nevertheless their study reveals certain of the magmatic processes more clearly and more in detail than do the simpler non-ore- bearing rocks. — The later stages of the evolution of the igneous rocks. This process finally develops a series of "acid extracts" which form pegmatite and aplite dikes, contact deposits (by the reaction of these extracts upon 1* Bowen, N. Their accumulation will be effected by different factors. Do the gaseous extracts react on the earlier minerals to form new minerals ; and is there in the later stages actual replacement of one substance by another? Note on the condition of platinum in the nickel-copper ores from Sudbury.

It has survived long enough for the copyright to expire and the book to enter the public domain. Brum Boezinger, Assistant Professor of Germanic Languages. Most of the examples I reported upon were adult ; and because the bone happened to be missing in a young individual of Mug U, the question was brought up as to whether it was not the ossified end of the tendon, that is always attached to it, developed with age. The thick sheet of tendon, that covers much of the inner part of this and the dorsal muscle, shallowly invades this muscle at about its middle, and along the plane of this invasion the muscle may be rather THE SESAMOID ARTICULAR 9 easily separated. For example, it is generally assumed that the segregation of the large bodies of iron ore in the Bushveldt laccolith in South Africa and in the Duluth laccolith and the sulfid masses in the Sudbury laccolith have been con- trolled by gravity.* Beyschlag, Krusch, and Vogt' state "Bei den meisten Eruptivge- steinen beginnt die Kristallisation mit der Aussonderung der sogenannten Erzmineralien, wie Magnetit oder Titanomagnetit, Eisenglanz, Ilmenit, Zirkon, Apatit, Schwefelkies, mitunter auch Spinel u. Vogt, who has examined the magmatic ores both in the field and with the microscope, favors the hypothesis that prior to the crys- tallization of the rock-minerals the ores separate as an immiscible sulfid or oxid melt, which continues in the molten state during the consolida- tion of the silicates, intrudes the latter, and finally crystallizes. Modem investigation of polished surfaces of ores has led to the discovery that the magmatic sulfid ore-minerals have a definite order of crystallization, and that the younger minerals intrude and replace the older.

A public domain book is one that was never subject to copyright or whose legal copyright term has expired. This seemed more probable at that time, as I was investigating the skeleton of Dallia in which the posttemporal ligament ossifies rather late in life. The inner part thus separated may represent A-3 of Vetter, and the outer part A-2. To meet this, Howe has framed a modification of Vog^'s hypothe- sis.

ORG Registry Domain ID: D103987416-LROR Registrar WHOIS Server: Registrar URL: Date: 2017-01-17TZ Creation Date: 2004-02-16TZ Registry Expiry Date: 2018-02-16TZ Registrar: Ascio Technologies, Inc. USA Registrar IANA ID: 106 Registrar Abuse Contact Email: [email protected] Abuse Contact Phone: 44.2070159370 Domain Status: ok https://icann.org/epp#ok Registry Registrant ID: AT1385503203271 Registrant Name: Rune Jensen Registrant Organization: Registrant Street: Houvej 292 Registrant City: Gandrup Registrant State/Province: Registrant Postal Code: 9362 Registrant Country: DK Registrant Phone: 45.50901711 Registrant Phone Ext: Registrant Fax: Registrant Fax Ext: Registrant Email: [email protected] Admin ID: AT24375096-051 Admin Name: Hostmaster Funktionen Admin Organization: A/S Admin Street: Kalvebod Brygge 45 Admin City: Copenhagen V Admin State/Province: Admin Postal Code: 1560 Admin Country: DK Admin Phone: 45.46907100 Admin Phone Ext: Admin Fax: 45.70205872 Admin Fax Ext: Admin Email: [email protected] Tech ID: AT35145166-015 Tech Name: Master Host Tech Organization: Tech Street: Kalvebod Brygge 24 Tech City: Copenhagen V Tech State/Province: Copenhagen V Tech Postal Code: 1560 Tech Country: DK Tech Phone: 45.46907100 Tech Phone Ext: Tech Fax: 45.70205872 Tech Fax Ext: Tech Email: [email protected] Server: NS01. Marks, notations and other maiginalia present in the original volume will appear in this file - a reminder of this book's long journey from the publisher to a library and finally to you. The captions are not at all coordinate in value, nor are they consistent in terminology. Dissecting this tendinous covering away a stout sesa- moid articular tendon is found, which comes from the lower part of the sheet of tendon, or the part covering the ventral muscle (A-2 3).. Weitere Untersuchungen iiber die Ausscheidungen von Titaneisenerzen in basischen Eruptivgesteine. None of the magmatic ores are entirely free from alteration, and in some cases they are associated with high-temperature alteration products as well as with those of hydrothermal origin. Usage guidelines Google is proud to partner with libraries to digitize public domain materials and make them widely accessible. For instance, the small orders of Ganoids together with the lung fishes are under one caption. Attached to the articular below the sesamoid articular and below Meckel's cartilage is a less compact bundle of tendinous fibers from the same source. We also acknowledge our indebtedness to Professor Bailey Willis for a critical reading of the manuscript and for valuable suggestions. It became necessary for us, therefore, to study the various stages of mineral deposi- tion, especially the migrations and alterations that follow the original deposition of the ore. Many other fishes were worked on, but to report on all of them does not appear to be of advantage to the present inquiry. Edwin Chapiu Starks, Assistant Professor of Zoology, 77 pp.. A few of the drawings and brief descriptions of the muscles are here presented, and show their diversity of form and position.

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