銆婂博鐭冲湴鐞冨寲瀛︺�嬭涔?/p>
-2
4
鐔旂浣滅敤
(liquation)
鎴栧博娴嗕笉娣锋憾浣滅敤
(melt immiscibility)
宀╂祮鍐峰嵈鎴栦笂鍗囧噺鍘嬫椂锛?/p>
鍘熸潵鍧囧寑鍗曠浉鐨勭啍浣撴湁鏃朵細鍒嗚В鎴愪袱涓垚鍒嗕笉鍚岀殑鐔斾綋鐩搞�?/p>
杩?/p>
涓�杩囩▼鎴愪负鐔旂浣滅敤
(liquation)
锛屽畠鏄敱宀╂祮鐨勪笉娣锋憾鎬ц川鎵�鍐冲畾鐨勩�傝繖涓�杩囩▼绫讳技浜庣⒈鎬?/p>
闀跨煶鐨勫嚭婧躲�傚垎瑁傜殑缁勫垎涓�涓亸閰告�т竴涓亸鍩烘�э紝鎴栬�呬竴涓槸瀵?/p>
Fe,Ni
纭寲鐗╃殑鐔斾綋锛堟湁鍒?/p>
浜庢垚鐭匡級
锛屼竴涓负纭呴吀鐩愬博娴嗐�傝繖閮ㄥ垎鐮旂┒鐩稿杈冨急锛堜竴浜涙儏鍐靛皢鍦ㄥ井閲忓厓绱犻儴鍒嗕粙缁嶏級
銆?/p>
5
宀╂祮娣峰悎浣滅敤
(mixing, mingling )
涓や釜鎴愬垎涓嶅悓鐨勫博娴嗗彂鐢熸贩鍚堬紝
鐢变簬娣峰悎鏂瑰紡鍜屾贩鍚堟瘮渚嬬殑宸紓涔熶娇娣峰悎褰㈡垚鐨勫博娴嗘垚
鍒嗘湁寰堝ぇ鐨勫彉鍖栥�?/p>
绂忓缓娌挎捣骞虫江宀涗笂鐨?/p>
I
鍨嬭姳宀楀博琚涓烘槸宀╂祮娣峰悎浣滅敤鐨勪骇鐗┿�?/p>
鍛ㄦ柊姘戝拰
钁ｄ紶涓囩瓑浠庨噹澶栧湴璐ㄥ锛?/p>
鐭跨墿瀛﹀拰宀╃煶鍦扮悆鍖栧璇佸疄浜嗚姳宀楄川宀╂祮鍙楀埌鐜勬璐ㄥ博娴嗘贩鍚堢殑瀛?/p>
鍦ㄣ�?/p>
6
娌夌Н宀╀腑鐨勬贩鍚堜綔鐢?/p>
(Mixing in sedimentary rocks)
Trends
on
variation
diagrams
for
sedimentary
rocks
may
result
from
the
mixing
of
the
different
ingredients
which
constitute
the
sediment.
Bhatia
(1983),
in
a
study
of
turbidite
sandstones
from
eastern
Australia,
shows
Harker
diagrams
in
which
there
is
a
change
in
mineralogical maturity, i.e. an increase in quartz coupled with a decreas in the proportions of lithic
fragments and feldspar (Fig 1-18).
Fig 1-18 Harker variation diagrams for quartz-rich sandstone suites from eastern Australia
(Bhatia,
1983).
The
increase
in
SiO
2
inflects
an
increased
mineralogical
maturity,
i.e.
a
greater
quartz content and a smaller proportion of detrital grains.
Argast and Donnelly (1987)
璁や负鍦ㄦ垚鍒嗗彉鍖栧浘涓婏紝濡傛灉浜屽厓缁勫垎锛?/p>
x
杞达紝
y
杞达級瀵嗗垏鐩?/p>
鍏筹紙绾挎�у彉鍖栵級
锛屽垯鍙兘鍙嶆槧鐨勬槸璇ュ娌夌Н宀╂槸鐢变袱绉嶇熆鐗╃粍鍒嗘贩鍚堢殑銆傚鐭宠嫳
鈥?/p>
浼婂埄鐭筹紝
鎴栭暱鐭?/p>
/
鐭宠嫳
鈥?/p>
浼婂埄鐭虫贩鍚堛�傚鏋滃彉鍖栨槸鏇茬嚎鎴栨棤瑙勫緥锛堝讥鏁ｇ殑锛?/p>
锛屽垯鍙兘鏄笁缁勫垎娣峰悎銆傚
鐭宠嫳
鈥?/p>
浼婂埄鐭?/p>
鈥?/p>
鏂硅В鐭炽�?/p>