structural-tectonic complex
81community ecology — Introduction study of the organization and functioning of communities (community), which are assemblages of interacting populations of the species living within a particular area or habitat. As populations of species interact with one …
82Levofloxacin — Systematic (IUPAC) name (S) 7 fluoro 6 (4 methylpiperazin 1 yl) 10 oxo 4 thia 1 azatricyclo[7.3.1.05,13] trideca 5(13),6,8,11 tetraene 11 carboxylic acid …
83Sirte Basin — The Sirte Basin is a late Mesozoic and Tertiary triple junction continental rift (extensional basin) along northern Africa that was initiated during the late Jurassic Period. It borders a relatively stable Paleozoic craton and cratonic sag basins …
84Geology of Indonesia — This is a brief summary of the geology of Indonesia. The details are stored in Wikibooks [http://en.wikibooks.org/wiki/The Geology of Indonesia] Tectonics The tectonics of Indonesia is very complex as it is a meeting point of several tectonic… …
85Himalayas — Himalayan, adj. /him euh lay euhz, hi mahl yeuhz/, n. the, a mountain range extending about 1500 mi. (2400 km) along the border between India and Tibet. Highest peak, Mt. Everest, 29,028 ft. (8848 m). Also called the Himalaya, Himalaya Mountains …
86Ceraunius Fossae — MOLA colorized image of Ceraunius Fossae region. The fractured terrain consists of two large patches of north south trending faults surrounded by lava flows. The Alba Mons volcano is the large, circular feature at top …
87Marshall Space Flight Center — George C. Marshall Space Flight Center Aerial view of the test area at MSFC …
88Zagros Mountains — Topographic map of Iran with the Zagros Mountains The Zagros Mountains from space, September 1992 …
89Evidence of common descent — The wide range of evidence of common descent of living things strongly indicates the occurrence of evolution and provides a wealth of information on the natural processes by which the variety of life on Earth developed, supporting the modern… …
90Passive margin — A passive margin is the transition between oceanic and continental crust which is not an active plate margin. It is constructed by sedimentation above an ancient rift, now marked by transitional crust. Continental rifting creates new ocean basins …
