| 000 | 02809nam a2200385 a 4500 | ||
|---|---|---|---|
| 005 | 20250918192305.0 | ||
| 008 | 130723s2013 gw ab b 001 0 eng c | ||
| 020 |
_a9783540882619 (alk. paper) _cRM569.26 |
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| 020 | _a3540882618 (alk. paper) | ||
| 039 | 9 |
_a201403051514 _bzaina _c201402191436 _drosli _c201402131547 _dros _y07-23-2013 _zros |
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| 040 |
_aUKM _cUKM _dYDXCP _dBTCTA _dOBE _dBWX _dDLC _dUKM |
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| 090 | _aQE613.G533 | ||
| 090 |
_aQE613 _b.G533 |
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| 100 | 1 | _aGlass, Billy P. | |
| 245 | 1 | 0 |
_aDistal impact ejecta layers : _ba record of large impacts in sedimentary deposits / _cBilly P. Glass, Bruce M. Simonson. |
| 260 |
_aHeidelberg : _bSpringer, _c2013. |
||
| 300 |
_axv, 716 p. : _bill. (some col.), maps ; _c24 cm. |
||
| 490 | 1 |
_aImpact studies, _x1612-8338 |
|
| 504 | _aIncludes bibliographical references (p. 641-705) and index. | ||
| 505 | 0 | _aIntroduction -- Impact crater formation, shock metamorphism, and distribution of impact ejecta -- Distal impact ejecta layers : recognition, confirmation, dating, and determining source craters -- Cenozoic microtektite/ejecta layers -- Mesozoic spherule/impact ejecta layers -- Paleozoic impact spherule/ejecta layers -- Proterozoic impact spherule/ejecta layers younger than 2.4 Ga -- Spherule layers near the Archean-Proterozoic boundary -- Paleoarchean spherule layers -- Modeling variations in distal impact ejecta/spherule layers through space and time -- Distal impact ejecta layers and earth history -- Appendix A : recovery of ejecta material from confirmed, probable, or possible distal ejecta layers. | |
| 520 | _a'Impact cratering is an important geological process on all solid planetary bodies, and, in the case of Earth, may have had major climatic and biological effects. Most terrestrial impact craters have been erased or modified beyond recognition. However, major impacts throw ejecta over large areas of the Earth's surface. Recognition of these impact ejecta layers can help fill in the gaps in the terrestrial cratering record and at the same time provide direct correlation between major impacts and other geological events, such as climatic changes and mass extinctions. This book provides the first summary of known distal impact ejecta layers.'--P. [4] of cover. | ||
| 650 | 0 | _aCryptoexplosion structures. | |
| 650 | 0 | _aCratering. | |
| 650 | 0 | _aSediments (Geology). | |
| 650 | 0 | _aGeology, Stratigraphic. | |
| 700 | 1 | _aSimonson, Bruce M. | |
| 907 |
_a.b15681968 _b2019-11-12 _c2019-11-12 |
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| 942 |
_c01 _n0 _kQE613.G533 |
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| 914 | _avtls003534947 | ||
| 990 | _ark4 | ||
| 991 | _aFakulti Sains dan Teknologi | ||
| 998 |
_at _b2013-10-07 _cm _da _feng _ggw _y0 _z.b15681968 |
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| 999 |
_c550822 _d550822 |
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