يعرض 31 - 40 نتائج من 94 نتيجة بحث عن '"Wei, Dongyan"', وقت الاستعلام: 0.67s تنقيح النتائج
  1. 31
    كتاب

    المصدر: Lecture Notes in Electrical Engineering ; China Satellite Navigation Conference (CSNC) 2018 Proceedings ; page 799-811 ; ISSN 1876-1100 1876-1119 ; ISBN 9789811300288 9789811300295

  2. 32
    كتاب

    المصدر: Lecture Notes in Electrical Engineering ; China Satellite Navigation Conference (CSNC) 2018 Proceedings ; page 537-549 ; ISSN 1876-1100 1876-1119 ; ISBN 9789811300288 9789811300295

  3. 33
    كتاب

    المصدر: China Satellite Navigation Conference (CSNC) 2017 Proceedings: Volume I ; Lecture Notes in Electrical Engineering ; page 495-512 ; ISSN 1876-1100 1876-1119 ; ISBN 9789811045875 9789811045882

  4. 34
    مؤتمر
  5. 35
    مؤتمر
  6. 36
    دورية أكاديمية
  7. 37
    كتاب

    المصدر: Lecture Notes in Electrical Engineering ; China Satellite Navigation Conference (CSNC) 2015 Proceedings: Volume III ; page 809-817 ; ISSN 1876-1100 1876-1119 ; ISBN 9783662466315 9783662466322

  8. 38
    كتاب

    المصدر: Lecture Notes in Electrical Engineering ; China Satellite Navigation Conference (CSNC) 2015 Proceedings: Volume III ; page 819-838 ; ISSN 1876-1100 1876-1119 ; ISBN 9783662466315 9783662466322

  9. 39
    كتاب

    المصدر: Lecture Notes in Electrical Engineering ; China Satellite Navigation Conference (CSNC) 2015 Proceedings: Volume III ; page 583-593 ; ISSN 1876-1100 1876-1119 ; ISBN 9783662466315 9783662466322

  10. 40

    المصدر: Acta Geologica Sinica - English Edition. 74:613-617

    الوصف: A water/salt system in an evaporative environment is both a physicochemical region and a biological one. All the parameters of the system, such as the salinity, temperature and CO2 partial pressure, are affected by halo-philic bacteria. The system controls salt deposition but is modified by an accompanying ecological system; therefore it should be called a water/salt/biological system. Salt minerals result from accumulation of the remains of bacteria/algae, namely, bacteria/algae formation; whereas biological, biophysical and biochemical processes provide full evidence for organic involvement. Consequently, salt deposits should not be called purely chemical but biological/chemical ones. This new argument supplements and develops the traditional idea and helps perfect the mineralization theory of salts and even general deposits, thus giving guidance to prospecting for salt deposits.