Copyright © Philip M. Parker, INSEAD. Terms of Use.
| Domain | Definition |
Mining | A characteristic of some minerals where substitution for one or more elements by others does not change the crystal structure. An example is the substitution of iron for zinc in sphalerite, wherein the iron content can range up to more than 15% without changing the sphalerite structure. Similarly, iron, manganese, and magnesium ions can replace each other inthe calcite structure common to siderite, rhodochrosite, and magnesite. (references) |
Source: compiled by the editor from various references; see credits. | |
Hexadecimal (or equivalents, 770AD-1900s) (references)49 53 4F 4D 4F 52 50 48 4F 55 53 52 45 50 4C 41 43 45 4D 45 4E 54 |
| Leonardo da Vinci (1452-1519; backwards) (references)
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Binary Code (1918-1938, probably earlier) (references)01001001 01010011 01001111 01001101 01001111 01010010 01010000 01001000 01001111 01010101 01010011 00100000 01010010 01000101 01010000 01001100 01000001 01000011 01000101 01001101 01000101 01001110 01010100 |
HTML Code (1990) (references)I S O M O R P H O U S   R E P L A C E M E N T |
ISO 10646 (1991-1993) (references)0049 0053 004F 004D 004F 0052 0050 0048 004F 0055 0053 0052 0045 0050 004C 0041 0043 0045 004D 0045 004E 0054 |
Encryption (beginner's substitution cypher): (references)435349474952504249555325239504635373947394854 |
| 1. Orthography 2. Bibliography |
Copyright © Philip M. Parker, INSEAD. Terms of Use.
