| LDR | | 00000nam u2200205 4500 |
| 001 | | 000000435048 |
| 005 | | 20200227113938 |
| 008 | | 200131s2019 ||||||||||||||||| ||eng d |
| 020 | |
▼a 9781392541470 |
| 035 | |
▼a (MiAaPQ)AAI27547981 |
| 040 | |
▼a MiAaPQ
▼c MiAaPQ
▼d 247004 |
| 082 | 0 |
▼a 338 |
| 100 | 1 |
▼a Smith, Joshua M. |
| 245 | 10 |
▼a Origins of Country Rock-Hosted Ni-Cu-Pge Massive Sulfides near Mafic-Ultramafic Intrusions of the North American Midcontinent Rift System and the Stillwater Complex. |
| 260 | |
▼a [S.l.]:
▼b Indiana University.,
▼c 2019. |
| 260 | 1 |
▼a Ann Arbor:
▼b ProQuest Dissertations & Theses,
▼c 2019. |
| 300 | |
▼a 216 p. |
| 500 | |
▼a Source: Dissertations Abstracts International, Volume: 81-06, Section: B. |
| 500 | |
▼a Advisor: Ripley, Edward M. |
| 502 | 1 |
▼a Thesis (Ph.D.)--Indiana University, 2019. |
| 506 | |
▼a This item must not be sold to any third party vendors. |
| 520 | |
▼a Igneous rock-hosted sulfides in mafic-ultramafic intrusions produce most of the world's nickel and PGEs. These sulfides were produced by sulfide saturation in mafic-ultramafic magmas and accumulation of sulfide liquid in the magmatic systems. Some massive Ni-Cu-PGE sulfides also occur in local country rocks. Within the Midcontinent Rift System, sheet-style and conduit-style intrusions host disseminated to massive sulfides in igneous rocks. Country rock-hosted massive Ni-Cu-PGE sulfides are also found near at least three Midcontinent Rift-related intrusions |
| 590 | |
▼a School code: 0093. |
| 650 | 4 |
▼a Geology. |
| 650 | 4 |
▼a Geochemistry. |
| 650 | 4 |
▼a Mining. |
| 690 | |
▼a 0372 |
| 690 | |
▼a 0996 |
| 690 | |
▼a 0551 |
| 710 | 20 |
▼a Indiana University.
▼b Geological Sciences. |
| 773 | 0 |
▼t Dissertations Abstracts International
▼g 81-06B. |
| 773 | |
▼t Dissertation Abstract International |
| 790 | |
▼a 0093 |
| 791 | |
▼a Ph.D. |
| 792 | |
▼a 2019 |
| 793 | |
▼a English |
| 856 | 40 |
▼u http://www.riss.kr/pdu/ddodLink.do?id=T15494516
▼n KERIS
▼z 이 자료의 원문은 한국교육학술정보원에서 제공합니다. |
| 980 | |
▼a 202002
▼f 2020 |
| 990 | |
▼a ***1008102 |
| 991 | |
▼a E-BOOK |