GWD6-Q23 to Q26: (鑽石題)
Diamonds are almost impos-
sible to detect directly because they
are so rare: very rich kimberlite
Line pipes, the routes through which
(5) diamonds rise, may contain only
three carats of diamonds per ton
of kimberlite. Kimberlite(講的是一種成色極佳的南非鑽石) begins as
magma in Earth’s mantle (the layer
between the crust and the core). As
(10) the magma smashes through layers
of rock, it rips out debris, creating
a mix of liquid and solid material.
Some of the solid material it brings
up may come from a so-called
(15) diamond-stability field, where condi-
tions of pressure and temperature
are conducive to the formation of
diamonds. If diamonds are to sur-
vive, though, they must shoot toward
(20) Earth’s surface quickly. Otherwise,
they revert to graphite or burn. 這裡是第一個重點,講的是說如果
沒有快速衝出地表,就會變成石墨或是燒掉了 Explorers seeking diamonds look
for specks of “indicator minerals”
peculiar to the mantle but carried up
(25) in greater quantities than diamonds
and eroded out of kimberlite pipes
into the surrounding land. The stan-
dard ones are garnets(石榴石), chromites(鉻鐵),
and ilmenites(鈦鐵). One can spend years
(30) searching for indicators and tracing
them back to the pipes that are their
source; however, 90 percent of
kimberlite pipes found this way are
barren of diamonds, and the rest
(35) are usually too sparse to mine. 這肯定是第二個重點,就是說透過一些方法來找,是可以勉強找到,但效果很差,不符成本原則 In the 1970’s the process of
locating profitable pipes was refined
by focusing on the subtle differ-
ences between the chemical
(40) signatures of indicator minerals
found in diamond-rich pipes as
opposed to those found in barren
pipes. For example, G10 garnets,
a type of garnet typically found in
(45) diamond-rich pipes, are lower in
calcium and higher in chrome than
garnets from barren pipes. (這裡有題,請特別留意)Geo-
chemists John Gurney showed that
garnets with this composition were
(50) formed only in the diamond-stability
field; more commonly found ver-
sions came from elsewhere in the
mantle. Gurney also found that
though ilmenites did not form in the
(55) diamond-stability field, there was a
link useful for prospectors: when
the iron in ilmenites was highly
oxidized(生鏽), its source pipe rarely
contained any diamonds.這裡是指,garnet總是出現在有鑽石的地方,而ilmenites要是生鏽,就不會有鑽石,iron有氧存在,就不是鑽石生長的地方He rea-
(60) soned that iron took on more or less
oxygen in response to conditions in
the kimberlitic magma itself—mainly
in response to heat and the avail-
able oxygen. When iron became
(65) highly oxidized, so did diamonds;
that is, they vaporized into carbon
dioxide. 就不是鑽石,而是蒸發為二氧化碳,注意最後一段的最後一句