ChonJeomnet |
2012-07-02 22:13:44 |
149 |
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However, in reality there is often a small amount of argon remaining in a rock when it hardens. This is usually trapped in the form of very tiny air bubbles in the rock. One percent of the air we breathe is argon. Any extra argon from air bubbles may need to be taken into account if it is significant relative to the amount of radiogenic argon (that is, argon produced by radioactive decays). This would most likely be the case in either young rocks that have not had time to produce much radiogenic argon, or in rocks that are low in the parent potassium. One must have a way to determine how much air-argon is in the rock. This is rather easily done because air-argon has a couple of other isotopes, the most abundant of which is argon-36. The ratio of argon-40 to argon-36 in air is well known, at 295. Thus, if one measures argon-36 as well as argon-40, one can calculate and subtract off the air-argon-40 to get an accurate age.
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susan2 |
2012-06-25 17:05:32 |
148 |
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hehaha, |
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jenny65 |
2012-06-24 05:10:21 |
147 |
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Wahooooo, |
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susan2 |
2012-06-24 04:58:12 |
146 |
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oh yes, |
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jamesy679p |
2012-06-23 22:26:47 |
145 |
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hehaha, |
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david6677ll |
2012-06-22 00:19:54 |
144 |
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oh boy, |
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kevinx55656 |
2012-06-20 11:17:18 |
143 |
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oh yes, |
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jenny65 |
2012-06-20 11:02:28 |
142 |
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hehaha, |
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susan2 |
2012-06-20 04:45:28 |
141 |
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oh yes, |
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marilyn dafa |
2012-06-09 15:32:00 |
140 |
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perfect work£¬i'm in beijing too£¬why not use sse to optimize the vector and matrix£¿or make an opencl version£¿ |
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